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  • 1
    Call number: 12021 ; 10/M 93.0073/1
    In: Developments in geochemistry
    Type of Medium: Monograph available for loan
    Pages: XVIII, 383 S.
    ISBN: 0444416366
    Series Statement: Developments in geochemistry 1
    Language: English
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  • 2
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/M 93.0208/7
    In: Developments in economic geology
    Type of Medium: Monograph available for loan
    Pages: XI, 280 S. : Ill., graph. Darst.
    ISBN: 044441567X
    Series Statement: Developments in economic geology 7
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Tulsa, Oklah. : American Association of Petroleum Geologists
    Associated volumes
    Call number: 9/M 93.0209
    In: AAPG studies in geology
    Type of Medium: Monograph available for loan
    Pages: VII, 196 S. : graph. Darst.
    ISBN: 0891810099
    Series Statement: AAPG Studies in geology 5
    Language: English
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  • 4
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/M 93.0251A/6
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 5
    Call number: G 7276 ; 4/M 93.0215
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: XII, 410 S. : graph. Darst.
    ISBN: 9027707944
    Series Statement: NATO ASI series : C, Mathematical and physical sciences 30
    Language: English
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  • 6
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/21
    In: CRREL Report, 78-21
    Description / Table of Contents: This study investigates the possibility of providing estimates of the time of occurrence and length of the freezing season for any location in East and West Germany by using the average Januavy air temperature (AJ AT) as an index. The results indicate that reliable values of the mean freezing index can be obtained from the AJAT relationships which are developed for Germany. This association is further verified using data from the northeastern part of the U.S., and the AJ AT is then used to determine the average starting and ending dates (and hence the probable length) of the freezing season for stations in Germany. The AJ AT and the average dates of snowfall occurrence for numerous locations in the U.S. and Germany are also correlated. Interrelationships between these parameters and the average number of days with snow on the ground for stations up to 3000 m in elevation in Germany are examined. A detailed AJ AT map for East and West Germany, in which data from 134 stations, latitude, altitude and regional influences are considered, is developed in order to make the relationships usable. A historical review of the literature on snow studies in Germany and a brief discussion of snow-cover interpretation by satellite photography are included
    Type of Medium: Series available for loan
    Pages: v, 48 Seiten , Illustrationen , 1 Karte
    Series Statement: CRREL Report 78-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Historical literature review Relationships between midwinter temperature and freezing season Mean freezing index 4 Average January air temperature U.S. comparative study Correlation of AJAT and duration of freezing season Relationships between average January air temperature and snow conditions U.S. relationships German relationships Mapping of average January air temperatures Analysis of observed AJ AT data Development of detailed maps Application and discussion Examples Influence of vegetation Literature cited Appendix A. interpretation of snow cover by satellite Appendix B. Contour, station elevation and Aj AT maps for East and West Germany
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  • 7
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/10
    In: CRREL Report, 78-10
    Description / Table of Contents: The compressibility of wet snow is described in terms of pressure melting and nonlinear viscous deformation at grain contacts. The results of experiments with different salinities and liquid water contents are compared with computed densities. The decreasing compressibility of wet snow with increasing salinity and decreasing liquid content is quantified and explained. Simultaneous particle growth and the doubly charged layer at phase boundaries are included in the model. The results show that the density of wet snow increases approximately as a power of time but is highly dependent on the stress, initial particle size, liquid water content, and ionic impurity content of the snow.
    Type of Medium: Series available for loan
    Pages: vi, 23 Seiten , Illustrationen
    Series Statement: CRREL Report 78-10
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Experimental procedure Grain growth Stressed particle contacts Fluid pressure Packing geometry Temperature distribution and heat flow Fluid and impurity flows Results The liquid film Conclusions Literature cited
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  • 8
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/16
    In: CRREL Report, 78-16
    Description / Table of Contents: A model investigation of drifting snow conditions was conducted in a hydraulic flume using a sand-water analog. Model results were evaluated to define modeling parameters that would allow quantitative correlation between measured prototype drift conditions and the model. The modeled structure was the standard plan snow fence designed by the Wyoming Highway Department and installed along Interstate Highway 80 in 1971. The performance of this system was documented by the Rocky Mountain Forest and Range Experiment Station of the U.S. Forest Service. Models of the fence were constructed for three heights and two geometric scales. Geometric scaling was based on terrain roughness and boundary layer thickness considerations, while velocity scaling was based on particle fall velocity and threshold of motion characteristics. Simulation of the atmospheric boundary layer was found to be of primary importance. Velocity scaling analysis suggested the use of a 'significant wind' concept based on a combination of velocity magnitude and frequency. Similarity of precipitation rate was not essential, and could be altered within limits to adjust the time scale. The response of the model to the shape of model elements was significant. Although the model is distorted and inexact similarity is achieved, it appears useful on a practical basis.
    Type of Medium: Series available for loan
    Pages: vi, 26 Seiten , Illustrationen
    Series Statement: CRREL Report 78-16
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Background Experimental design Similitude considerations The model Model operation Results Velocity Fence height Porosity Model correlation Summary and conclusions Recommeqdations for future work Literature cited Appendix A
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  • 9
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/15
    In: CRREL Report, 78-15
    Description / Table of Contents: This report first discusses the general approach for calculating the horizontal forces an ice cover exerts on a structure. Ice force determination consists of two parts: (1) the analysis of the in-plane forces assuming that the ice cover remains intact and (2) the use of a failure criterion, since an ice force cannot be larger than the force capable of breaking up the ice cover. For an estimate of the largest ice force, an elastic plate analysis and a failure criterion are often sufficient. A review of the literature revealed that, in the majority of the analyses, it is assumed that the failure load is directly related to a 'crushing strength' of the ice cover. However, observations in the field and tests in the laboratory show that in some instances the ice cover fails by buckling. This report reviews the ice force analyses based on the buckling failure mechanism and points out their shortcomings. The report then presents a new method of analysis which is based on the buckling mechanism
    Type of Medium: Series available for loan
    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 78-15
    Language: English
    Note: CONTENTS Abstract Preface Introduction and statement of problem Review of relevant analyses and tests Determination of the largest ice force on an isolated structure Preliminary remarks The buckling analysis of a floating wedge Proposed method to determine Literature cited
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  • 10
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/14
    In: CRREL Report, 78-14
    Description / Table of Contents: The analytical solution and the numerical study of the eigenvalue problem for determining the buckling pressure of an infinite elastic plate floating on water and stressed uniformly along the periphery of an internal hole is presented. The boundary conditions considered are the clamped-, simple-, and free-edge conditions. Small buckling pressure occurs only for the free-edge condition. The shape of the deflection for the free-edge condition suggests that buckling is an important mechanism of failure.
    Type of Medium: Series available for loan
    Pages: v, 55 Seiten , Illustrationen
    Series Statement: CRREL Report 78-14
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction 1. The problem 2. Abstract of the result Part I. Fundamental solutions 3. Fuchsian type solutions 4. Contour integral solution 5. Integration of the integral solution 6. Fundamental solutions for α = 1 7. Fundamental solutions for α = 0 8. Eigenvalues for α = 0 9. Fundamental solutions for α 〉 1 Part II. Asymptotic expansions 10. Asymptotic expansion for 0 〈 α ⩽1 11. Asymptotic expansion for 1 ≦ α ≦ 2 12. Asymptotic expansion for 2 ≦ α ≦ ∞ Part III. Eigenvalues 13. Range of eigenvalues 14. Eigenvalues for the free-edge condition 15. Eigenvalues for the clamped-edge and simple-edge conditions 16. Deflection Acknowledgement Literature cited Appendix A. Analytical continuation at the singular point Appendix B. Tensorial transformations Appendix C. Comparison of the semi-infinite plate buckling with the asymptotic buckling
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  • 11
    Call number: ZSP-201-78/12
    In: CRREL Report, 78-12
    Description / Table of Contents: Road test sections of membrane-enveloped silt and clay soils overlain with asphalt cement concrete were subjected to repetitive dynamic plate-bearing loadings to determine their strength variations during freeze-thaw cycles. The recoverable surface deformations in the load deflection bowl were continuously measured during the loading cycles and analyzed using the Chevron layered elastic computer program to obtain the in situ resilient deformation modulus of the various section layers at different stages of the freeze-thaw cycles. The resilient stiffness of the pavement system (the total load per unit of resilient load plate deflection) was also calculated for the various freeze-thaw conditions. The modulus values of the asphalt cement concrete varied inversely with its temperature by an order of magnetide (90,000 psi to 1,300,000 psi). The resilient stiffness of the pavement system varied in the same manner by nearly a factor of eight (228.4 kips/in. to 1740.2 kips/in.). Despite the wide strength variations of the sections during freeze-thaw cycles, membrane-enveloped fine-grained soils can be utilized instead of granular materials as base and subbase layers in flexible pavements in cold regions where moisture migration is a major concern. Moisture migration did not occur at saturation levels up to 75%, thus there was no strength loss during thawing.
    Type of Medium: Series available for loan
    Pages: v, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 78-12
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S.customary to metric units of measurement Introduction Freeze-thaw system Construction materials Controlled environment test section Outdoor sections Temperature monitoring instrumentation Repetitive plate bearing test apparatus Test results and analyses Conclusions Literature cited
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/13
    In: CRREL Report, 78-13
    Description / Table of Contents: Field observations of the growth fabrics of the fast and near-fast ice along the coasts of the Beaufort and Chukchi Seas show that, at depths of more than 60 cm below the upper ice surface, the sea ice crystals show striking alignments within the horizontal plane. At one site this alignment was well developed at a depth of 15 cm and in all cases the degree of preferred orientation increased with depth, with the strongest orientations occurring at the bottom of the ice sheet. In general the c-axes of the crystals were aligned roughly E-W parallel to the coast. In the vicinity of islands the alignment roughly paralleled the outlines of the islands and in narrow passes between islands the alignment paralleled the channel. Our observations, as well as similar observations made in the Kara Sea by Cherepanov, can be explained if it is assumed that the c-axes of the crystals are aligned parallel to the 'long-term' current direction at the sea ice/sea water interface. The alignments are believed to be the result of geometric selection among the growing crystals, with the most favored orientation being that in which the current flows normal to the (0001) plates of ice that make up the dendritic ice/water interface characteristics of sea ice. It is hypothesized that current flow in this direction reduces the thickness of the solute boundary layer as well as the salinity in the liquid at the interface. This lowered salinity allows crystals in the favored orientation to extend farther into the melt than neighboring crystals with less favored orientations. In addition the current tends to induce a continuous flux of supercooled seawater against the sides of the crystals that extend ahead of the interface.
    Type of Medium: Series available for loan
    Pages: v, 29 Seiten , Illustrationen
    Series Statement: CRREL Report 78-13
    Language: English
    Note: CONTENTS Abstract Preface Introduction Locale and techniques Observations Vertical variations in crystal orientation Regional variations in crystal orientation Summary of observations Causes Initial ice skim Earth’s magnetic field Currents Conclusions and consequences Literature cited
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  • 13
    Call number: ZSP-201-78/28
    In: CRREL Report, 78-28
    Type of Medium: Series available for loan
    Pages: x, 112 Seiten , Illustrationen
    Series Statement: CRREL Report 78-28
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Introduction Descriptions of road test sections Test equipment and procedures Field repetitive plate bearing tests Data analysis General Layered-elastic analysis of the pavement systems Statistical analysis Flexural analysis Summary and conclusions Literature cited Appendix A: Resilient surface deflections for the test points
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  • 14
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/22
    In: CRREL Report, 78-22
    Description / Table of Contents: Special environmental factors that influence the design, laying and maintenance of undersea pipelines and cables in polar waters are described. Various approaches to the protection of submarine pipes and cables are considered, and prime emphasis is given to burial techniques for shallow water. A wide range of methods for trenching and burying are discussed, and technical data are given.
    Type of Medium: Series available for loan
    Pages: v, 36 Seiten , Illustrationen
    Series Statement: CRREL Report 78-22
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors Introduction Types of pipelines and cables Potential hazards to pipelines and cables Areas of concern Waterdepth Sea ice Icebergs and ice islands Submarine permafrost Ice gouging Seabed erosion by water jets Protection methods Protection of unburied pipes and cables Protection by burial Backhoe digging Wireline equipment Plowing and ripping from the surface Plowing and ripping by self-propelled seabed vehicles Bucket ladder dredges Suction dredging Conventional cutterhead dredges Low pressure water jetting Bottom-traveling cutterhead dredges Explosive methods Novel methods Disc saws, wheel ditchers and milling drums Ladder trenchers and chain saws Repetitive impulse devices High pressure water jets Flame jets and plasma torches Electrical discharge and electromagnetic radiation Chemical methods Conclusions Literature cited
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  • 15
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/27
    In: CRREL Report, 77-27
    Description / Table of Contents: The spectral reflectance of natural snow in the range of 0.20- to about 0.40-micrometers wavelengths was studied in the laboratory using both continuous spectral scanning and fixed bandpass measurements. White barium sulfate pressed powder was used as a standard for comparison. The reflectance of fresh snow was found to be very high (usually nearly 100%) and only weakly wavelength dependent from 0.24 micrometers to the visible range. In the 0.20- to 0.24-micrometers portion of the spectrum, the reflectance was found to be quite erratic. Possible reasons for the irregularities in reflectance measurements are discussed.
    Type of Medium: Series available for loan
    Pages: v, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 77-27
    Language: English
    Note: CONTENTS Abstract Preface Introduction Experimental procedure Snow collection Spectrophotometric methods Data analysis Potential sources of error Presentation of results Continuous-scan measurements Comparison of sequential bandpass and continuous-scan measurements Theoretical calculations Discussion of results Differences in amplitude of reflectance measurements Irregularities in the shape of spectral reflectance curves The true spectral reflectance of snow in the ultraviolet region Conclusions Literature cited Appendix A. Absolute reflectance values of pressed BaSO4 powder
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  • 16
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/21
    In: CRREL Report, 77-21
    Description / Table of Contents: Cold weather limits the successful application of built-up roofing, but often a roof installation must be completed late in the fall or in the winter. The loose-laid protected membrane roof with a synthetic sheet membrane can be installed in the middle of the winter with complete reliability. A synthetic membrane is traditionally more expensive than built-up roofing (rising crude oil prices, however, have reversed this condition), but it has two special features besides its suitability for winter installation: it can be placed on a damp deck, if necessary, and, being losse-laid, it does not split because of deck movement. This report documents information on the installation of two roofs in Anchorage, Alaska, during January and February 1972, including a discussion of the necessary snow removal from the bare deck and the use of portable shelters for preparing the lap joints between sheets during very cold weather. The winter installation caused no special construction problems and the advantages of the synthetic membrane make it an attractive alternative to built-up roofing. The cost of loose-laid protected membrane roofs in Alaska was, in 1972, nearly $300 per square ($28/sq.m), including insulation. Prices are rising as labor costs rise and as more insulation is specified.
    Type of Medium: Series available for loan
    Pages: 5 Seiten , Illustrationen
    Series Statement: CRREL Report 77-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction The protected membrane roof Winter construction considerations Construction costs Conclusion
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  • 17
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/19
    In: CRREL Report, 77-19
    In: Mechanics of cutting and boring, Part VI
    Description / Table of Contents: Abstract: The report deals with forces and power levels in cutting machines having adisc or drum that rotates about an axis perpendicular to the direction of advance. The forces on individual cutting tools are related to position on the rotor and to characteristics such as tool layout, rotor speed, rotor size, machine advance speed, and rotor torque. Integration leads to expressions for force components acting on the rotor axis, taking into account tool characteristics, cutting depth of the rotor, and rotor torque. These provide estimates of tractive thrust and thrust normal to the primary free surface. For self-propelled machines, this leads to considerations of traction, normal reaction, weight and balance, and power/weight ratios. Specific energy consumption is analyzed and related to machine characteristics and strength ofthe material being cut. Power per unit working area is discussed, and data for existing machines are summarized. Power requirements for ejection ofcuttings are analyzed, and the hydrodynamic resistance on underwater cuttings is treated. A number of worked examples are given to illustrate the principles discussed in the report.
    Type of Medium: Series available for loan
    Pages: vii, 36 Seiten , Illustrationen
    Series Statement: CRREL Report 77-19
    Language: English
    Note: CONTENTS Abstract Preface Foreword Introduction Terminology Forces on individual cutters Torque force and tool force Forces on the rotor axis Tractive thrust and down thrust Alternative tool force formulations Vehicle traction Power/weight ratio Weight and balance Force, torque, speed and power Specific energy Efficiency and performance index Power density Power requirements for ejection of cuttings Hydrodynamic resistance in underwater cutting
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  • 18
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/18
    In: CRREL Report, 77-18
    Description / Table of Contents: Abstract: Models originally developed to describe the arching and the movement of granular materials through hoppers or chutes are applied to the arching and drift of pack ice in straits and gulfs having lengths of 50 to 500 km. Verification of the usefulness of the models is attempted by making comparisons with ice deformation patterns as observed via satellite imagery in the Bering Strait region and in Amundsen Gulf. The results are encouraging in that there is good correspondence between observed arching and lead patterns and those predicted by theory. In addition, values determined via the model for the angle of internal friction (≈ 30° to 35°) and the cohesive strength per unit thickness (≈ 2000 N/m) are similar to values obtained by other approaches. It is estimated that if the wind velocity parallel to the Bering Strait exceeds ≈ 6 m/s, there will be ice flow through the strait.
    Type of Medium: Series available for loan
    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 77-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theory Limiting span of an arch Flow of pack ice through converging channels Stoppage of flow Applications St. Lawrence Amundsen Gulf Bering Strait Conclusion References
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  • 19
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/16
    In: CRREL Report, 77-16
    Description / Table of Contents: A brief discussion is given of the ways an icebreaker breaks ice. Since the icebreaking process is so complex, the solution of a mathematical model does not appear to be feasible. As an alternative, it is suggested that physical models be used to design icebreakers. The appropriate scaling laws for physical models are developed and their practical limitation discussed.
    Type of Medium: Series available for loan
    Pages: ii, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 77-16
    Language: English
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  • 20
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Associated volumes
    Call number: G 7148(2. Ex.) ; 10/G 7724 ; M 93.0092/12 ; G 7148(1. Ex.)
    In: Minerals and rocks
    Type of Medium: Monograph available for loan
    Pages: IX, 229 S. : graph. Darst.
    Series Statement: Minerals and rocks 12
    Language: English
    Location: Upper compact magazine
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  • 21
    Call number: 9/M 93.0055/7
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: XII, 475 S.
    Series Statement: Developments in precambrian geology 7
    Language: English
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  • 22
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/27
    In: CRREL Report, 78-27
    Description / Table of Contents: Uniaxial compression and tension tests were conducted on polycrystalline snow-ice to determine the effect of temperature on its strength. Test temperatures ranged from -O.1C to -54C. Two machine speeds, 0.847 mm/s and84.7 mm/s were used for the constant displacement rate tests. The compressive strength at -54C was about oneorder of magnitude higher than at -0.1C. The tensile strength at -18C was about 20% higher than at 0.1C. The initial tangent and 50% strength moduli are given for the compression tests, while the secant modulus to failure is given for the tension tests.The mode of fracture is discussed and the test results are compared with data from other investigations.
    Type of Medium: Series available for loan
    Pages: iii, 22 Seiten , Illustrationen
    Series Statement: CRREL Report 78-27
    Language: English
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  • 23
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/19
    In: CRREL Report, 78-19
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 78-19
    Language: English
    Note: CONTENTS Abstract Preface Introduction Previous work Methods and results Methods of analysis Salinity-chlorophyll a associations Discussion Comparison of ice and water column standing crops Estimated mass of ice associated chl. a Mechanism of ice algae formation in the Weddell Sea Differences between the biological environments of fast and drifting pack ice Conclusions Literature cited Appendix A. Species variations - ice and water column
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  • 24
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/26
    In: CRREL Report, 78-26
    Description / Table of Contents: Ice fog suppression experiments on the Fort Wainwright Power Plant cooling pond were conducted during the winters of 1974-76. Baseline information studies occupied a sizable portion of the available ice fog weather in 1974-75. Then hexadecanol was added to the pond and dramatically improved visibility by reducing fog generated from water vapor released by the pond at -14 C. Although this temperature was not low enough to create ice fog, the cold vapor fog created was equally as devastating to visibility in the vicinity of the pond. During the winter of 1975-76, suppression tests were continued using films of hexadecanol, mixes of hexadecanol and octadecanol, and ethylene glycol monobutyl ether (EGME). Suppression effectiveness at colder temperatures was stuided and limits to the techniques were probed. A reinforcing grid was constructed that prevented breakup of the film by wind and water currents. Lifetime tests indicated that EGME degrades much more slowly than either hexadecanol or the hexadecanol-octadecanol mix. The films were found to be very effective fog reducers at warmer temperatures but still allowed 20% to 40% of normal evaporation to occur. The vapor thus produced was sufficient to create some ice fog at lower temperatures, but this ice fog occurred less frequently and was more quickly dispersed than the thick fog that was present before application of the films.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 78-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Ice fog from cooling ponds Evaporation Relative humidity and cold air Ice fog suppression Air movement Plastic films Rafts Injection wells Cooling towers Chemical films Reinforced film experiments Meteorological data collection Floating reinforcement grid Application of the hexadecanol film Hexadecanol, octadecanol mixes Ethylene glycol monobutyl ether Laboratory tests of suppression effectiveness Conclusions Literature cited Appendix A. Design for an automatic thin chemical film applicationsystem Appendix B. Meteorological data
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  • 25
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/18
    In: CRREL Report, 78-18
    Description / Table of Contents: The primary objective of this project was to demonstrate the utility of remote sensing techniques as an operational tool in the acquisition of data required by the U.S. Army Corps of Engineers, Seattle District, in the Grays Harbor dredging effects project, and related projects. Aerial imagery was used to map surface circulation and suspended sediment patterns near the hopper dredge pump site at the harbor entrance and near pulpmill outfalls in Aberdeen, and to map the areal distribution and extent of intertidal habitats. The surface circulation maps prepared from the aerial photographs and thermal imagery compared favorably with the large-scale circulation patterns observed in the Grays Harbor hydraulic model at the U.S. Army Engineer Waterways Experiment Station. Of the imagery provided by NASA, the thermal imagery was more useful than the color or color infrared (CIR) photographs for mapping circula­tion, while the CIR photographs were more useful than the thermal imagery or the color photographs for mapping intertidal habitats. Current velocities estimated from dye dispersion patterns and drifting dye drogues were comparable at some locations to velocities measured by in situ current meters and in the hydraulic model. Based on a cursory evaluation of LANDSAT-1 imagery acquired in January, February, and October 1973, it had limited utility in providing data on surface circulation patterns in Grays Harbor. The areal distribution and extent of nine wetland vegetation types, dune vegetation, and three types of eelgrass were mapped using primarily aerial C IR photographs and ground sur­veys. Color photographs were also used for areas not covered by the C IR photographs. Wetland vegetation types mapped were: low silty marsh, low sandy marsh, sedge marsh, high immature marsh, high mature marsh, salt marsh, diked pasture, freshwater marsh, and wooded swamp. Undiked salt marsh (first five types) covered 5540 acres (22.3 km2) in Grays Harbor.
    Type of Medium: Series available for loan
    Pages: vi, 85 Seiten , Illustrationen
    Series Statement: CRREL Report 78-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Site description Background and objectives Project history Approach General Aircraft imagery and sensor data LANDSAT imagery Ground truth data Results and discussion Remote sensing techniques Conventional techniques Comparison of results Conclusions Advantages and disadvantages Applications Recommendations Literature cited
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  • 26
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/8
    In: CRREL Report, 77-8
    Description / Table of Contents: A broadbanded impulse radar system was used for aerial detection of accumulated frazil and brash ice in a 9.5-km reach of the St. Lawrence River near Ogden Island. The remote sensing and data reduction system developed for the project provided data sufficient for production of a contour map having 1-ft intervals. With this contour map, the accumulation pattern of frazil and brash ice could be analyzed. Recommendations are given for improving the performance of the aerial profiling system.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 77-8
    Language: English
    Note: CONTENTS Page Abstract Preface Conversion factors: U.S. customary to metric (SI) units of measurement Background Objectives Profiling system Approach Profiling method Data reduction and interpretation Results Conclusions Recommendations Literature cited Appendix A. Comparison of ground and aerial data
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  • 27
    Call number: ZSP-201-77/9
    In: CRREL Report, 77-9
    Description / Table of Contents: This report presents experimental results on the conditions of initiation of an ice jam by a simple surface obstruction, on the equilibrium thickness of an ice jam formed by accumulation and submergence of ice floes, and on the compression strength of floating, fragmented ice cover. In the study on ice jam initiation, it was found that the minimum concentration of floes in the opening of the obstruction at which a jam occurs is nearly independent of the ratio of width of constricted passage to channel width, and is proportional to a negative power of the ratio of floe length to width of constricted passage. From energy analysis of floe submergence, a relationship relating the thickness of a jam formed by accumulation and submergence of floes to the approach flow characteristics was derived and found to fit satisfactorily the experimental data. In experiments on compression strength of floating, fragmented ice cover it was found that the compressive strength is inversely proportional to compression velocity and independent of cover length.
    Type of Medium: Series available for loan
    Pages: vii, 45 Seiten , Illustrationen
    Series Statement: CRREL Report 77-9
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Introduction I. Initiation of ice jams by partial surface obstructions A. Introductory remarks B. Experimental apparatus and procedure C. Dimensional analysis D. Presentation of results and discussion ΙΙ. Thickness of ice jams due to accumulation and transport of ice floes A. Introductory remarks B. Experimental apparatus and procedures C. Presentation of results E. Conclusion III. Compressive strength of floating fragmented ice covers A. Introductory remarks B. Experimental setup and procedure C. Presentation of results and discussion D. Conclusions Literature cited Appendix A: Experimental results on ice jam initiation Appendix B: Effect of surface tension on submergence velocity of ice floes Appendix C: Experimental results for ice jam thickness study Appendix D: Experimental results on compressive strength of fragmented ice cover
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  • 28
    Call number: ZSP-201-78/9
    In: CRREL Report, 78-9
    Description / Table of Contents: Large, simply supported beams of temperate lake ice were found, generally, to yield significantly higher flexural strengths than the same beams tested in the cantilever mode. Data support the view that a significant stress concentration may exist at the fixed corners of the cantilever beams. Maximum effects are experienced with beams of cold, brittle ice substantially free of structural imperfections; for this kind of ice the strength difference factor, here attributed to the effect of stress concentrations, may exceed 2.0; that is, simply supported beams test a factor of 2 or more stronger than the same beams tested in the cantilever mode. In ice that has undergone extensive thermal degradation, the stress concentration effect may be eliminated entirely. Simply supported beams generally yield higher strengths when the top surfaces are placed in tension. This behavior is attributed to differences in ice type; the fine-grained, crack-free top layer of snow-ice which constituted up to 50% of the ice cover in the current series of tests usually reacted more strongly in tension than the coarse-grained crack-prone bottom lake ice.
    Type of Medium: Series available for loan
    Pages: iv, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 78-9
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test sites and ice cover properties Beam testing Results Discussion Conclusions Literature cited
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  • 29
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/2
    In: CRREL Report, 78-2
    Description / Table of Contents: Many of the technical questions relating to iceberg transport are given brief, but quantitative, consideration. These include iceberg genesis and properties, the mechanical stability of icebergs at sea, towing forces and tug characteristics, drag coefficients, ablation rates, and handling and processing the iceberg at both the pick-up site and at the final destination. In particular the paper attempts to make technical information on glaciological and ice engineering aspects of the problem more readily available to the interested planner or engineer. Specific conclusions include: (1) No unprotected iceberg, no matter how long or wide, would be likely to survive the ablation caused by a long trip to low latitudes. (2) Icebergs that have a horizontal dimension exceeding 2 km may well be prone to breakup by long wavelength swells. (3) To avoid the dangers associated with an iceberg capsizing, the width of a 200-m thick iceberg should always be more than 300 m. (4) For towing efficiency the length/width ratio of a towed iceberg should be appreciably greater than unity. (5) For a pilot project, the selected iceberg would have to be quite small, if for no other reason than the practical availability of tug power.
    Type of Medium: Series available for loan
    Pages: v, 31 Seiten , Illustrationen
    Series Statement: CRREL Report 78-2
    Language: English
    Note: CONTENTS Abstract Preface Introduction Sources and properties of tabular icebergs Sources Characteristics of ice shelves near the ice front Characteristics of tabular icebergs Towing Geophysical and engineering considerations Tug characteristics Handling and processing Cutting and boring with thermal devices Penetration with electrothermal devices Electrothermal cutting Making vertical cuts by pre-split blasting Primary fragmentation by blasting Primary fragmentation by mechanical sawing Comminuting ice with machines Slurry pipelines Conclusion Literature cited
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  • 30
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/17
    In: CRREL Report, 77-17
    Description / Table of Contents: A literature search was made for information on the accretion of ice on ocean structures and on methods for control. The bulk of the reports were in Russian, with some additional Japanese, British, American, Canadian, and Icelandic sources. Analysis of icing reports indicated that sea spray is the most important cause of ship icing, with lesser amounts due to freezing rain, snow, and fog. Icing is a potential danger whenever air temperatures are below the freezing point of water and the sea temperature is 6 C or lower. Theoretical work on the ice accretion process is discussed, and a method is suggested, based on Russian experiments, for calculating the sea spray accumulation rate for cylindrical and flat surfaces as a function of water source temperature, air temperature, and wind speed. Other factors that influence icing severity are ship size and configuration, angle between ship course and water heading, and ship speed. Icing in the north temperate latitudes generally occurs in the rear of barometric depressions. Maps showing limits of various degrees of icing severity are included. Atmospheric icing measurements on tall land-based structures are presented, and potential maximum accumulations estimated. Control measures are discussed, though no completely effective method is available. Mechanical (impaction) methods are the most common, but experiments have been conducted on heated, icephobic, and deformable surfaces, and with freezing point depressants. No device for the unequivocal measurement of ice accumulation is available, though some experimental methods are suitable for controlled testing; it is recommended that a device be developed.
    Type of Medium: Series available for loan
    Pages: v, 42 Seiten , Illustrationen
    Series Statement: CRREL Report 77-17
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric units of measurements Introduction The freezing proeess Icing observations Geographical distribution of icing and contributing meteorological conditions Extreme icing conditions Extremes of icc accumulation Prediction of icing occurrences Prediction of icing intensity and rate Control methods Measurement of icing rate Conclusions and recommendations Literature cited Appendix A. Maps of icing occurrence and rate Appendix B. Data for computing ship icing rates Appendix C. Estimation of ice accumulation
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  • 31
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/12
    In: CRREL Report, 77-12
    Description / Table of Contents: A computer program to calculate the increased live load on a snow-covered roof due to rain-on-snow is given. For the 25-year rainstorm falling on a heavy snow load on a flat roof in Hanover, New Hamsphire, and additional 98 kg/m2 (20 lb/ft2) of liquid water is added to the live load. The additional load due to rain-on-snow is very sensitive to the snow properties and characteristics of the roof. A wide range of live loads is possible, depending on the particular circumstances.
    Type of Medium: Series available for loan
    Pages: vii, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 77-12
    Language: English
    Note: CONTENTS Page Abstract Preface Summary Nomenclature Introduction Water movement through snow Vertical percolation Lateral flow Flat roofs Sloping roofs Rainfall intensity-duration effects Miscellaneous effects Radial flow to drains Flow along gutters on snow-covered roofs Snow structure Basal layer Conclusion Literature citied Appendix A. Computer program calculating roof loads from rain-on-snow
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  • 32
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/14
    In: CRREL Report, 77-14
    Description / Table of Contents: The breakup of the Chena River was observed and documented during the spring of 1975 and 1976. This study attempted to determine the potential for damage to the proposed Chena River flood control dam from ice and debris during breakup. Results of this study were compared to those of a 1974 companion study. In 1975, ice thickness were determined to be 15% thinner than in 1974 and ice volume was 33% smaller. No major ice floes were observed in 1975 and no significant flooding occurred, although the approaches to a bridge at the damsite were eroded by debris and high water immediately after breakup. The 1976 breakup was milder than that of 1975. Minor flooding in the lower river was caused by jamming of a few large ice pieces, but no property damage resulted.
    Type of Medium: Series available for loan
    Pages: v, 44 Seiten , Illustrationen
    Series Statement: CRREL Report 77-14
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Ice thickness and quantity Chronology of the 1975 Chena River breakup Checkpoint 3 Checkpoint 4 Checkpoint 5 Checkpoint 6 Checkpoint A Checkpoint 7 Checkpoint C Checkpoint D Checkpoint 8 Checkpoint 10 Checkpoint 11 Checkpoint 12 Spring flooding and debris The 1976 Chena River breakup Breakup in other years Summary and conclusions Appendix A. Sequential photographs of 1975 breakup at checkpoints 3-12
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  • 33
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-77/15
    In: CRREL Report, 77-15
    Description / Table of Contents: A laboratory experimental study was conducted on a scale model of an annular flow ice-water heat sink to be used to store the waste heat produced in a hardened defense installation operating in an isolated mode. The study ex­amined: 1) scaling relationships for predicting the performance of prototype units using data from scale models, 2) the accuracy of a computer prediction technique developed during an earlier study, 3) the heat transfer phenom­enon at the ice-water interface, and 4) some practical aspects related to the operation of a prototype installation. The scaling relationships and the computer program were found to be sufficiently accurate for use in developing a proto­type sink design. During operation the scale model sink provided an almost constant low temperature source of coolant water for approximately one-half its useful life and thereafter behaved like an ordinary stored water reservoir type heat sink. No significant operational problems were discovered.
    Type of Medium: Series available for loan
    Pages: vii, 54 Seiten , Illustrationen
    Series Statement: CRREL Report 77-15
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Conversion factors: U.S. customary to metric units of measurement Introduction Description of experiment Apparatus Test procedure Experimental results Summary of experimental tests Influence of coolant water flow rates Approximation of the rate of melting Comparison of experimental and computed results Comparative analysis of the model sinks Approximation of the heat transfer coefficient Conclusions and recommendations Literature cited Appendix A. Experimental data, heat sink Model II Appendix B. Heat sink scaling and similarity relationships Appendix C. Derivation of the relationships for the heat transfer coefficient, Reynolds and Nusselt numbers Appendix D. Determination of freezing rates and refrigeration loads Appendix E. Approximation of stresses in the heat sink tank
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  • 34
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/11
    In: CRREL Report, 77-11
    Description / Table of Contents: Two performance indicators, effectiveness and thermal efficiency, are defined and used to evaluate the year-round performance of three protected membrane roofs in Alaska and New Hampshire. Effectiveness is a measure of the deviations of ceiling temperatures from a yearly average, with large diviations indicating erratic performance in the roofing-insulation system and small departures indicating a thermally stable system. Thermal efficiency, the ratio of calculated heat loss to measured heat loss, is affected by climatic conditions such as rain, snow, solar radiation and wind. Thermal efficiency values of 100% or greater are possible since the calculated heat loss is based only on the inside and outside air temperature differences and the thermal properties of the roof components. Results of the year-round evaluation indicate that the three protected membrane roofs generally have high values of both effectiveness and thermal efficiency.
    Type of Medium: Series available for loan
    Pages: v, 40 Seiten , Illustrationen
    Series Statement: CRREL Report 77-11
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S.customary to metric (SI) units of measurement Introduction Location of test sites Fairbanks Anchorage Hanover, N.H. Test program Instrumentation Effectiveness Therma lefficiency Heat balance within the roof Comparisons with conventional systems Conclusions Effectiveness of the test roof Thermal efficiency Heat balance within the roof Applicability Recommendations Literature cited Appendix A. Temperature and heat flow measurements, Anchorage and Fairbanks, Alaska, and Hanover, New Hampshire Appendix B. Thermal efficiencies of the test roof, Anchorage and Fairbanks, Alaska, and Hanover, New Hampshire Appendix C. January 1973 and August 1972 comparisons of protected membrane and conventional built-up membrane systems at Hanover, New Hampshire
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  • 35
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-77/10
    In: CRREL Report, 77-10
    Description / Table of Contents: Abstract: The amount of force that an ice sheet can apply to a vertical pile was tested by lowering a hydraulic ram device into a hole cut in an existing ice sheet. The device had a large base and shoved a relatively narrow vertical pile in a horizontal direction. Test variables were: pile widths - 1.5 in. to 36.7 in.; pile shapes - flat, round, 45 ° and 90° wedges; ice thickness - 2.6 in. to 8.8 in.; and ram speed - 0.07 in./sec to 18.75 in./sec; but not all shapes and sizes were tested at all speeds. Air temperature was 20 ° F (-6.7 ° C). Forces and displacements were measured electronically. The findings are presented as a table of test results and as bar graphs of the resultant ice pressures versus the pile width-to-ice-thickness ratio, pile width and shape combination and pile velocity. The types of failures in the ice sheet were classified as crushing, splitting, buckling, bending, and creeping. The ice sheet generally withstood a high initial load followed by several lower peak load levels. The maximum ice pressure measured was 610 psi for a 12.6-in.-diam round pile in 8.4-in.-thick ice.
    Type of Medium: Series available for loan
    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 77-10
    Language: English
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  • 36
    Call number: 9/MR 90.1102 ; MR 90.1103 ; M 93.0055/1
    In: Developments in precambrian geology
    Type of Medium: Monograph available for loan
    Pages: VIII, 406 S. : graph. Darst.
    Series Statement: Developments in precambrian geology 1
    Language: English
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  • 37
    Monograph available for loan
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    Berlin [u.a.] : Springer
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    Call number: 10/M 93.0251A/2
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 38
    Monograph available for loan
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    Berlin [u.a.] : Springer
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    Call number: 10/M 93.0251/3
    In: Handbook of geochemistry
    Type of Medium: Monograph available for loan
    Pages: Losebl.-Ausg.
    Language: English
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  • 39
    Call number: 4/M 90.1063 ; M 93.0062
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: XXV, 782 S.
    ISBN: 9027726183
    Series Statement: NATO ASI series : C, Mathematical and physical sciences 218
    Language: English
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  • 40
    Call number: M 93.0154/5 ; 11/G 9206
    In: Developments in petrology
    Type of Medium: Monograph available for loan
    Pages: XI, 272 S.
    ISBN: 0444416587
    Series Statement: Developments in petrology 5
    Language: English
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  • 41
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/24
    In: CRREL Report, 78-24
    Type of Medium: Series available for loan
    Pages: v, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 78-24
    Language: English
    Note: CONTENTS Abstract Preface Introduction Comparison of winters Ship effects Measured forces Sequential breaking of the structure Discussion Conclusions Recommendations Literature cited Appendix A. Force level fluctuations in west ice boom, 20 January 1977
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  • 42
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/20
    In: CRREL Report, 78-20
    Description / Table of Contents: Abstract: Measurements of the concentrations of Aitken nuclei in maritime air were made near Barrow, Alaska, in June 1975 with a modified Nolan-Pollack small-particle detector. The concentrations varied from 50 to 300 particles cm^-3 depending upon meteorological conditions. The mean Aitken nuclei count was 100 particles cm^-3 for diameters greater than 2 x 10^-3 μm. Transmission electron micrographs of aerosols in maritime air near Barrow were taken. The size range was measured to be 0.01 to 2.5 μm in diameter with the most frequently observed diameter being 0.04 μm. The volume of the maritime air and the collection efficiency of aerosol particles on filmed grids for electron microscopy were measured. The aerosol concentrations were found to be 76 to 101 particles cm^-3 ; the mean concentration was calculated to be 87 particles cm^-3. The aerosol particles in the maritime air were identified by electron microscopy and selected area electron diffraction analysis. About 20% of the aerosol particles were identified, and 80% of the particles were too small for electron diffraction analysis. Sea salt particles constituted 2% of the total, and clay minerals 3%; these particles were considered to be of natural origin. Solid combustion by-products such as coagulated carbon particles and fly ash particles constituted 16%. Despite the comparative remoteness of the sampling site, the measurements indicate that many anthropogenic aerosols were found using an electron microscope.
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    Pages: iv, 48 Seiten , Illustrationen
    Series Statement: CRREL Report 78-20
    Language: English
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  • 43
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-78/8
    In: CRREL Report, 78-8
    Description / Table of Contents: The interaction of a 5.1-GHz transverse electric surface wave with a dielectric slab is experimentally investigated. The wave is initially supported by a dielectric substrate resting upon a metallic ground-plane. A slab, made of the same dielectric material as the substrate and variable in height, is then placed upon the waveguide. The results for a small slab sitting on the substrate showed that the discontinuity was a very inefficient launcher of reflected surface waves. Investigations of these reflections with a trough waveguide showed that, for values of slab height comparable to the exponential decay height of the surface wave, the reflections remain very small. However, as the slab height is increased beyond the decay height, the reflected amplitude approaches the theoretical value for a plane wave reflected from the interface between air and the same dielectric. The results are applicable to surface wave methods of microwave deicing of wings and helicopter rotors.
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    Pages: v, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 78-8
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Background Objective and procedure Theory of plane surface waves Waveguide design and characteristics Physical apparatus Frequency characteristics Spatial distribution of Ey above the guide Guide wave length Surface wave interaction with a slab discontinuity Experiments with a trough Discussion and conclusions Literature cited
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  • 44
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/5
    In: CRREL Report, 78-5
    Description / Table of Contents: The viscoelastic deflection of an infinite floating ice plate subjected to a circular load was solved, assuming the Maxwell-Voigt type four-element model. An effective method of numerical integration of the solution integrals was developed, of which each integrand contains a product of Bessel functions extending to infinity. The theoretical curve was fitted to the field data, but the material constants thus found varied with time and location.
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    Pages: iii, 32 Seiten , Illustrationen
    Series Statement: CRREL Report 78-5
    Language: English
    Note: CONTENTS Abstract Preface Introduction The problem The solution Method of numerical integration Ramp/steady loading Curve fitting to time lapse deflections Asymptotic deflection Deflection profiles Acknowledgement Literature cited Appendix I. Analytical background Appendix II. Computer programs, ramp time profiles and steady time profiles
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  • 45
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/6
    In: CRREL Report, 78-6
    Description / Table of Contents: A new freezing mechanism, called segregation freezing, is proposed to explain the generation of the suction force that draws pore water up to the freezing surface of a growing ice lens. The segregation freezing temperature is derived by applying thermodynamics to a soil mechanics concept that distinguishes the effective pressure from the neutral pressure. The frost-heaving pressure is formulated in the solution of the differential equations of the simultaneous flow of heat and water, of which the segregation freezing temperature is one of the boundary conditions.
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    Pages: iv, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 78-6
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature Introduction Segregation freezing Analysis Heat conduction in the nascent ice layer Water flow in the unfrozen soil Heat transfer in the unfrozen soil Energy balance at the segregation-freezing front Numerical computation Literature cited Appendix A. Essence of Portnov’s method Appendix B. Frost-heaving without air available
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  • 46
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-78/1
    In: CRREL Report, 78-1
    Description / Table of Contents: The results of axial double point-load tests on disk samples of snow and ice obtained from the area of McMurdo Sound, Antarctica, are presented. They show the effects of temperature, sample length, load point diameter and specific gravity on failure load. It was determined that 13 samples should be tested to obtain a representative mean strength index. The results show that the axial double point-load test has good possibilities as a rapid field test for determining the unconfined comrpessive strength of snow and ice but that further evaluation of the variables affecting test results must be made.
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    Pages: iii, 11 Seiten , Illustrationen
    Series Statement: CRREL Report 78-1
    Language: English
    Note: CONTENTS Abstract Preface Introduction Test procedure Test program Test samples Number of test for determining strength index Effect of temperature Effect of sample length Effect of load point size Tests on snow Discussion Recommendations Literature cited
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  • 47
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-77/31
    In: CRREL Report, 77-31
    Description / Table of Contents: Ten roofs in Concord, New Hampshire, were surveyed for wet insulation using a hand-held infrared camera. Suspected wet areas were marked on the roof with spray paint and roof samples were obtained to verify wet and dry conditions. Recommendations for maintenance and repair were made based on infrared findings, water contents, and visual examinations. An incremental economic study is presented to serve as a guide in determining the most cost-effective approach.
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    Pages: v, 29 Seiten , Illustrationen
    Series Statement: CRREL Report 77-31
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: US, customary to metric (SI) units of measurement Introduction Infrared camera Core samples State House State House Annex State Library Legislative Office Building Public Health Complex Highway Garage Fish and Game Offlces Supreme Court John O. Morton Building Department of Health and Welfare Laboratory Economics of roof reinsulation Conclusions and recommendations Literature cited
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  • 48
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-77/7
    In: CRREL Report, 77-7
    In: Mechanics of cutting and boring, IV
    Description / Table of Contents: The report deals with the cutting of rock and similar materials by parallel motion tools. It examines cutting forces and energy requirements, taking into consideration tool geometry, wear, operating conditions, and material properties. After an introductory discussion of terminology, some general principles are outlined, and relevant theoretical ideas on metal cutting and rock cutting are reviewed. The next section, which is the heart of the report, reviews experimental data on the magnitudes and directions of cutting forces. There is a graphical compilation of data, including some from obscure or unpublished sources. The variables covered include chipping depth, rake angle, relief angle, side rake, base angle, tool width, tool compliance, tool speed, tool wear, tool interactions, and material properties. The second major part of the report treats the energetics of cutting. It begins with a short discussion of relevant principles, and continues with a compilation and review of experimental data, covering the same independent variables as the force section. The report ends with a concise summary of general behavior for parallel motion tools.
    Type of Medium: Series available for loan
    Pages: xi, 85 Seiten , Illustrationen
    Series Statement: CRREL Report 77-7
    Language: English
    Note: CONTENTS Abstract Preface Foreword Introduction Terminology Principles of cutting Forces acting on a single cutter Theoretical Ideas on cutting Experimental data on cutting forces Effect of chipping depth on tool forces Effect of rake angle on tool forces Effect of relief angle on cutting forces Effect of side rake on tool forces Effect of base angle or face profile on tool forces Effect of rounding at the cutting edge Effect of tool width on cutting forces Tool compliance and force fluctuations Effect of tool speed on cutting forces Effect of rock properties on cutting forces Tool interaction and kerf spacing Effect of multiple pass cutting on tool forces Effect of tool wear on cutting forces Development of wear Energetics of cutting Energetics of parallel-motion tools Variation of specific energy with chipping depth for a single tool Effect of rake angle on specific energy Effect of relief angle on specific energy Effect of side rake on specific energy Effect of base angle or face profile on specific energy Effect of tip radius on specific energy Effect of tool width on specific energy Effect of tool speed on specific energy Variation of specific energy with rock properties Effect of kerf spacing on specific energy Effect of multiple pass cutting on specific energy Effect of tool wear on specific energy General summary Literature cited Appendix Α. Additional data for ice Appendix Β. Conversion factors: U.S. customary and metric units of measurement
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  • 49
    Call number: 21/SR 90.0917(52/1) ; MOP 44444 / Mitte ; 21/SR 22.19544(52/1)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 52, Teil 1
    Description / Table of Contents: This 3rd International Symposium "Geodesy and Physics of the Earth" was according to its tenor the continuation of the Symposia of 1970 and 1973 dealing with the same basic topic. It was especially devoted to the possibilities of Satellite Geodesy to study geodynamic processes. By this also those problems of the use of observations of artificial satellites for geodetic and geophysical purposes were dealt with that had regularly been treated in the preceding years and will be treated further by A. Massevitsch in the symposia presided by her. Several papers were devoted especially to the problems of the Special Study Group 5.49 of the International Association of Geodesy "Use of Geodetic Data for Studies of Earth-Moon-System" (President E. Tengström). Part 1 : Papers of the Plenary Sessions
    Type of Medium: Series available for loan
    Pages: 232 Seiten , Illustrationen , 30 cm
    Edition: Als Manuskript gedruckt
    ISSN: 0514-8790
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 52, Teil 1
    Language: English , Russian
    Note: Preliminary remarks Papers of the Plenary Sessions Kautzleben, Heinz: Some Actual Problems in the Interpretation of Geodynamic Processes Massevitsch, A. G.: Results of Co-Operation in Section 6 of the Intercosmos Program Chovitz, Bernard H.: Monitoring Geodetic Networks by Space Techniques Mather, R. S.: Some Possibilities for Recovering Oceanographic Information from the SEASAT Missions Burša, Milan: Some Problems on the Dynamics of the Earth-Moon-System Treder, Hans-Jürgen: Nach-Newtonsche Korrekturen zur Dynamik des Systems Erde - Mond und ihre Bedeutung für die relativistischen Gravitationstheorien Eržanov, Z. S.: Secular Polar Motion of the Earth and its Parameters Computation from Artificial Satellites Observations Pellinen, L. P.: 1 Recent Possibilities for the Determination of the Geopotential from Terrestrial and Satellite Data Vyskočil, Pavel: Some Relationships between Vertical Recent Movements of the Earth's Surface and Deep Crustal Structure Bulygina, O. M.; Surnin, Ju. V.; Tatevjan, S. K.: Использование Метода "Коротких Дуг" для Опредения Координат Наземных Станций Montag, Horst; Gendt, Gerd: Coordinate Determination of Stations of the "Large Chords" Project by the Semidynamic Method Balmino, Georges; Reigber, Christoph; Moynot, Bernard: Further Evaluation of the GRIM 2 Earth Gravity Field Model
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  • 50
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: 5/M 92.1329(42)
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: IX, 187 S.
    ISBN: 0875900690
    Series Statement: Geophysical monograph 42
    Classification:
    Petrophysics
    Language: English
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    Monograph non-lending collection
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    New York : Wiley-Interscience
    Associated volumes
    Call number: 19/M 92.1361/3
    In: Encyclopedia of statistical sciences
    Type of Medium: Monograph non-lending collection
    Pages: ix, 722 S.
    ISBN: 0471055492
    Classification:
    C.1.7.
    Language: English
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  • 52
    Call number: 21/SR 90.0917(77) ; 21/SR 22.19544(77)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 77
    Type of Medium: Series available for loan
    Pages: 228 Seiten , Illustrationen, Karten , 30 cm
    ISSN: 0514-8790
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 77
    Language: English , Russian , German
    Note: Vorwort/Preface part I: Development and spatial position of molasses and their region of accumulation Lützner, H.; Vass, D.: Subdivision and stages of development of Variscan and Alpine molasses (on the base of the example of Central European Variscides and West Carpathians) Vass, D.; Krystek, I.; Stranik, Zd.: Tectonic activity in time of formation of Main and Late molasses in Czechoslovakian West Carpathians Vozarova, A.; Vozar, J.: Subdivision and stages of development of Variscan molasse of the Czechoslovakian West Carpathians Schwab, G.: The transition between molasse stage and platform cover in the Variscan Central Europe Волочкоич, К.Л. : Верхнепалеозойские орогенные комплексы и структуры Южного Тянь-Шаня (Late Paleozoic orogenic complexes and structures of Southern Tjan-Schan) Леонов, Ю.Г. ; Щерба, И.Г. : Некоторые особенности верхенекайнозойских моласс в зпиплатформенной активизации юга Средней Азии (Some features of Upper Cenozoic molasee in area of epi-platform reactivation in southern Middle Asia) Щерба, И.Г. : Характерный механизм образовация олистостромов в эпоху горообразования (Typical mechanism of olistostrome formation in orogenic epochs) Леонов, Ю.Г. : Корреляция тектонических движений в орогенных областях (областях молассообразования) и за их пределами (Correlation of tectonic movements within and outside of orogene regions (regions of molasse formation) part II: Geological development of block-tectonics in the region of Elbe-Lineament, especially in the territory of G.D.R. Bankwitz, P.; Frischbutter, A.; Bankwitz, E.: Structure and tectonic development of Elbe-zone Ludwig, A.O.: Die strukturelle Entwicklung des NW-Abschnittes des Elbe-Lineaments und Vergleich mit dem anschließenden SE-Abschnitt im Gebiet der DDR (The structural development of the NW-part of Elbe-lineament and comparison with the south-eastern part on the territory of G.D.R.) Benek, R.: Über Beziehungen des permosilesischen Vulkanismus zum Bruchmuster, speziell zum Elbe-Lineament (On relations of Permo-Silesian volcanism to the fault pattern, especially to the Elbe-lineament) Stackebrandt, W.: Zum tektonischen Charakter der Harznordrandstörung (On tectonic character of Northern Harz border fault system) Janssen, Chr.: Analyse der Spannungsverteilung im Tafeldeckgebirge des Subherzynen Beckens und angrenzender Gebiete (Investigations of distribution of paleostress in platform cover of Subhercyn basin and adjacent regions) Fusan, O.; Kvitkovič, J.; Plancǎr, J.: Bau und Dynamik einiger Blöcke der Westkarpaten (Structure and dynamics of several tectonic blocke of the West Carpathians) Николаев, В.Г.: Консолидированная земная кора паннонского бассейна (The consolidation of earth's crust in the Pannonian Basin)
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  • 53
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 92.0613
    In: Reviews in mineralogy
    Description / Table of Contents: In October 1975 a Short Course on Feldspar Mineralogy was held at the Hotel Utah, Salt Lake City, in conjunction with the annual meetings of the Mineralogical Society of America. Richard A. Yund, David B. Stewart, Joseph V. Smith and Paul R. Ribbe presented workshops on x-ray single-crystal and powder diffraction methods and electron optical techniques as applied to the study of feldspars and presented eight lectures, the substance of which became the nine chapters of the first edition of Feldspar Mineralogy. That book was published by the Mineralogical Society as the second volume of its series entitled Short Course Notes. In 1980 the MSA renamed the series Reviews in Mineralogy to more accurately reflect the scope and contents of the volumes, some of which -- including Volume 5 (1st and 2nd editions), this volume and a forthcoming one on fluid inclusions --were written without presentation at a short course. It will be noted by readers experienced with feldspars that there are many new ideas appearing in Chapters 3, 4 and 5 that have neither received scrutiny by review (other than ourselves) nor survived practical tests of time in the research community. There is some danger in this, but the editor decided the greater risk was to produce a review volume soon to be outdated. Inevitably, given the different goals of individual authors in their assigned topics, some repetition of material has occurred, although usually with quite different emphases. Chapters 1, 2, 9 and 10, in which plagioclase structures and diffraction patterns and their Al,Si distributions, phase equilibria and exsolution textures are featured, are notable in this regard. The editor has attempted to cross-reference these and as many other subjects throughout the volume as feasible. This is a luxury not afforded in other books of this series produced with a short course deadline, and it, together with the detailed Table of Contents, compensates to some degree for the lack of an index. Throughout this book repeated references are made to Smith (1974a,b); these are Volumes 1 and 2 of Feldspar Minerals, an encyclopedic work written by Joseph V. Smith and published by Springer-Verlag. We are particularly indebted to Drs. Konrad Springer and H. Wiebking for permission to reproduce many figures free of charge. The editor (and hopefully this volume) benefitted greatly from numerous stimulating discussions with David B. Stewart, some of which reached a high pitch, none of which came to blows, and several of which produced some palpable scientific progress. Stewart read and criticized many of the chapters. The authors are grateful to numerous individual scientists for figures, for data in advance of publication, and for encouragement and correction.
    Type of Medium: Monograph available for loan
    Pages: xii, 362 S.
    Edition: 2nd ed.
    ISBN: 0-939950-14-6 , 978-0-939950-14-0
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 2
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Chemistry, Structure, and Nomenclature of Feldspars by Paul H. Ribbe, p. 1 - 20. Chapter 2. Aluminum-Silicon Order in Feldspars: Domain Textures and Diffraction Patterns by Paul H. Ribbe, p. 21 - 56. Chapter 3. Lattice Parameters, Composition, and Al/Si Order in Alkali Feldspars by Herbert Kroll and Paul H. Ribbe, p. 57 - 100. Chapter 4. Lattice Parameters and Determinative Methods for Plagioclase and Alkali Feldspars by Herbert Kroll, p. 101 - 120. Chapter 5. Optical Properties of Feldspars by David B. Stewart and Paul H. Ribbe, p. 121 - 140. CHapter 6. Subsolidus Phase Relations in the Alkali Feldspars with Emphasis on Coherent Phases by Richard A. Yund and Jan Tullis, p. 141 - 176. Chapter 7. Microstructure, Kinetics and Mechanisms of Alkali Feldspar Exsolution by Richard A. Yund, p. 177 - 202. Chapter 8. Diffusion in Feldspars by Richard A. Yund, p. 203 - 222. Chapter 9. Phase Equilibria of Plagioclase by Joeseph V. Smith, p. 223 - 240. Chapter 10. Exsolution Textures in Ternary and Plagioclase Feldspars; Interference Colors by Paul H. Ribbe, p. 241 - 270. Chapter 11. Color in Feldspars by Anne M. Hofmeister and George R. Rossman, p. 271 - 280. Chapter 12. Some Chemical Properties of Feldspars by Joseph V. Smith, p. 281 - 296. Chapter 13. Deformation of Feldspars by Jan Tullis, p. 297 - 324. Appendix. Guides to indexing Feldspar Powder Patterns p. 325 - 342.
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    Call number: 21/SR 90.0917(78)
    Type of Medium: Series available for loan
    Pages: 172 S.
    Edition: Als Ms. gedr.
    Series Statement: Veröffentlichungen des Zentralinstituts für Physik der Erde 78
    Language: English
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  • 55
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    Berlin [u.a.] : Springer
    Associated volumes
    Call number: 10/G 9045
    In: Minerals and rocks
    Type of Medium: Monograph available for loan
    Pages: XII, 291 S. : graph. Darst.
    ISBN: 3540176675
    Series Statement: Minerals and rocks 19
    Language: English
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  • 56
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    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/G 9183
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: VIII, 472 S. : graph. Darst.
    ISBN: 0444421297
    Series Statement: Developments in sedimentology 36
    Language: English
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  • 57
    Series available for loan
    Series available for loan
    Berlin : Nationalkomitee für Geodäsie und Geophysik bei der Akademie der Wissenschaften der DDR
    Associated volumes
    Call number: Q 2453(II,28) ; MOP Per 581(2/28) ; ZSP-319/B-28
    In: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre, Heft 28
    Type of Medium: Series available for loan
    Pages: 136 Seiten , Illustrationen
    Series Statement: Geodätische und geophysikalische Veröffentlichungen : Reihe 2, Solarterrestrische Beziehungen und Physik der Atmosphäre 28
    Language: English
    Note: Content: Improvement of the coulometric measurement of ozone in the near-ground layer of the atmosphere / W. Warmbt. - Some experimental data on the variability of the ozone density at different level of the lowest atmosphere / A. G. Amiranashvili ; T. G. Gzirishvili ; A. I. Kartsivadse ; A. M. Okudjava ; D. F. Kharchilava ; K. H. Grasnick. - Report on the intercomparison of instruments measuring ozone near the ground at the Hohenpeissenberg Observatory / W. Warmbt. - Some results of ozone-sonde ascents in the CSSR / J. Picha. - A system of monitoring the observation and calibration qualities of Dobson spectrophotometerswithin the Regional Association VI / P. Plessing. - Vertical ozone distribution over Lindenberg (52.22°N, 14.12°E), 1975 - 1982 / U. Feister ; P. Plessing ; K. H. Grasnick. - Correlations of the total ozone with thermal and dynamic processes in the atmosphere / M. Frimescu ; L. Manea. - Numerical simulation of seasonal-latitudinal and 11-year variations in ozonosphere composition based on the two-dimensional photochemical model / I. G. Dyominov ; A. M. Zadorozhny. - Ozone content variation over central Europe and stratospheric dynamics in late winter / G. Entzian ; K. H. Grasnick. - Long-term ozone variation / G. Entzian ; K. H. Grasnick.
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  • 58
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    Berlin [u.a.] : Springer
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    Call number: 19/O 4313(1265)
    In: Lecture notes in mathematics
    Type of Medium: Monograph available for loan
    Pages: 201 S.
    ISBN: 3540180230
    Series Statement: Lecture notes in mathematics 1265
    Language: English
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  • 59
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    Orlando [u.a.] : Academic Press
    Associated volumes
    Call number: 9/M 454/1
    In: The techniques of modern stuctural geology
    Type of Medium: Monograph available for loan
    Pages: xiii, 307 S.
    ISBN: 0125769210
    Classification:
    Tectonics
    Language: English
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  • 60
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    Berlin [u.a.] : Springer
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    Call number: 4/G 8963
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: 183 S.
    ISBN: 3540179372
    Series Statement: Lecture notes in earth sciences 9
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    Berlin [u.a.] : Springer
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    Call number: 4/G 8965
    In: Lecture notes in earth sciences
    Type of Medium: Monograph available for loan
    Pages: 272 S. : Ill., graph. Darst.
    ISBN: 3540177108
    Series Statement: Lecture notes in earth sciences 10
    Language: English
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  • 62
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    New York [u.a.] : Elsevier
    Call number: 15/M 92.0946
    Type of Medium: Monograph available for loan
    Pages: xiv, 532 S.
    ISBN: 0444011803
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 63
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    Associated volumes
    Call number: 13/MR 97.0450(4A)
    In: The ocean basins and margins
    Type of Medium: Monograph available for loan
    Pages: XIII, 503 S.
    ISBN: 0306377748
    Language: English
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  • 64
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 13/MR 97.0450(4B)
    In: The ocean basins and margins
    Type of Medium: Monograph available for loan
    Pages: XIV, 445 S.
    ISBN: 0306377799
    Language: English
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  • 65
    Call number: Q 2435/39 ; ZSP-319/C-39
    In: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde, 39
    Type of Medium: Series available for loan
    Pages: 180 Seiten , Illustrationen
    ISSN: 0435-6187
    Series Statement: Geodätische und Geophysikalische Veröffentlichungen : Reihe 3, Physik der festen Erde 39
    Language: German , English
    Note: Inhalt Vorwort 1. Beiträge zu den geologisch orientierten Arbeitsgruppen 4, 7, 9 1.1. OLSZAK, G.: Zur strukturellen Umformung der Erdkruste bei der Entwicklung regionaler tektonischer Elemente 1.2. PAECH, H.-J.: Kurzer Tätigkeitsbericht über geologische Arbeiten in der westlichen Antarktis (Shackleton Range) 1.3. JUBITZ, K.-B.: Die Entwicklung des Amadeus-Beckens in Zentralaustralien - Beckendynamik im Bereich alter Tafeln 1.4. TESCHKE, H.-J.: Sarmato-Turan-Lineament 1.5. SCHROEDER, E.: Probleme der Entwicklung und des Baues der Varisziden in Mitteleuropa und im Gebiet der UdSSR 1.6. SOHROEDER, E.: Beiträge zur vergleichenden Analyse tektonischer Strukturen im Variszikum des Südurals und Mitteleuropas 1.7. SCHWAB, G.; BENEK, R.; BRÜCKNER, W.; JUBITZ, K.-B.; LUDWIG, A.; MEIER, R.; NÖLDEKE, W.; STOLL, A.; TESCHKE, H.-J.: Beckendynamik der Norddeutsch-Polnischen Senke - Paläomobilität im Bereich einer jungen Tafel (Fortschrittsbericht) 1.8. JUBITZ, K.-B.; TESCHKE, H.-J.: Das IGCP-Projekt 86 "SW-Rand der Osteuropäischen Tafel" und seine Beziehungen zum Geodynamik-Projekt 1.9. KRAUSS, M.: Ein Beitrag zur paläotektonischen Abgrenzung, Gliederung und Entwicklung des westlichen Teils der Osteuropäischen Plattform während des Paläozoikum (Gebiet Dänemark - Baltikum) 1.10. LÜTZNER, H.: Sedimentation, Vulkanismus und Tektonik der variazischen Innenmolasse im Thüringer Wald - Studien zur Paläomobilität im Übergangsstockwerk zwischen Geosynklinal- und Tafeletappe im Gebiet der DDR 1.11. LÄCHELT, S.: Geologisch-tektonisch-magmatische Entwicklung und metallogenetische Prozesse 1.12. KRAMER, W.: Zu einigen basischen magmatischen Formationen im Gebiet der DDR und deren geotektonischer sowie metallegenetischer Bedeutung 1.13. RÖSLER, H.J.; WERNER, C.-D.: Variazische Initialmagmatite Mitteleuropas 1.14. BENEK, R.: Vulkanit-Formationen als Indikatoren der Krustenfelderung bzw. unterschiedlichen Mobilitätsverhaltens 1.15. BANKWITZ, P.: Überblick über Magmatismus und Metamorphose im Altpaläozoikum Mittel- und Westeuropas 1.16. LÄCHELT, S.: Beziehungen zwischen der Blocktektonik, dem Magmatismus und der endogenen Metallogenie im mitteleuropäischen Raum 1.17. PAECH, H.-J.: Zum Ablauf tektogener Deformationen im mitteleuropäischen Variszikum 1.18. BANKWITZ, P.; BANKWITZ, E.; FRISCHBUTTER, A.: Zur Tektonik des Präkambriums der Elbezone und ihres Rahmens 1.19. BENEK, R.; FRISCHBUTTER, A.; NEUMANN, W.: Methodische Arbeiten im Kristallin des Baikal-Riftes 1.20. NEUMANN, W.: Paläogeographie und Paläotektonik des Nossen-Wilsdruffer Schiefergebirges (Saxothuringikum im Bereich des Zentralsächsischen Lineamentes) 1.21. LUDWIG, A.O.: Paläogeographie und Paläotektonik des Saxen von Mitteleuropa 1.22. MEIER, R.: Halogenese und Beckendynamik 1.23. BANKWITZ, P.; BANKWITZ, E.: Geologische Interpretation rezenter Krustenbewegungen Osteuropas 1.24. LUDWIG, A.O.: Zum gegenwärtigen Stand der Quartärforschung im südlichen Ostseeraum - Paläogeographie, Neotektonik, Aussagen zur Paläotektonik 1.25. ELLENBBRG, J.; FALK, F.; GRUMBT, E.; LÜTZNER, H.: Methodik der Untersuchungen von Molassen 1.26. NEUMANN, W.: Geologisches Modell zur Interpretation des tiefenseismischen NW - SE-Profils zwischen Granulit- und Erzgebirge 2. Beiträge zu der geophysikalisch-geodätisch orientierten Arbeitsgruppe 5 2.1. BÖLSCHE, J.; KRESSER, K.-D.: Erste Ergebnisse reflexionsseismischer Tiefenerkundung auf einem Profil von 30 km Länge im Süden der DDR 2.2. GRÄSSL, S.; HURTIG, E.; GRÜNTHAL, G.: Untersuchungen zum Bau der Erdkruste mit Hilfe seismischer Dreikomponentenregistrierungen 2.3. SCHULZE, A.: Untersuchungen zur Auflösung von Interferenzstrukturen seismischer Wellen mit Hilfe von Polarisationsfiltern 2.4. GROSSER, H.: Einfluß der Geometrie seismischer Punktwellen auf den Spektralinhalt des Wellenfeldes 2.5. STILLER, H.; WAGNER, F.C.; VOLLSTÄDT, H.: Die Geschwindigkeiten elastischer Wellen im klüftigen Gestein und in Erdbebengebieten 2.6. GRÜNTHAL, G.; HURTIG, E.: Zur .makroseismischen Auswertung des Friaul-Erdbebens vom 6. Mai 1976 auf dem Territorium der DDR 2.7. NEUNHÖFER, H.: Observation of microearthquakes in the Vogtland region since 1962 2.8. MAAZ, R.: Zur Statistik von Erdbeben 2.9. ELSTNER, CL.; HARNISCH, G.; ALTMANN, W.: Präzisionsgravimetrische Messungen auf der W - E-Linie der DDR 1970-76 2.10. FISCHER, H.; NEUBERT, R.: Instrumentelle Entwicklungen auf dem Gebiet der Laser-Satellitenentfernungsmessung 2.11. MONTAG, H.; GENDT, G.: Zur Untersuchung geodynamischer Parameter mit Hilfe von Satellitenbeobachtungen 2.12. JOCHMANN, H.: Betrachtungen zur Variation einiger Parameter der Polbewegung 2.13. HÖPFNER, J.: Untersuchungen von Amplituden- und Phasenänderungen der CHANDLER-, Jahres- und Halbjahreswelle 2.14. ARNOLD, K.: Einige Betrachtungen zum Auftreten und zur Bedeutung von Lateralinhomogenitäten der Dichte im Erdinneren 2.15. WALZER, U.: Report on mantle convection 2.16. SEIPOLD, U.: Messungen der thermischen Eigenschaften von Gesteinen unter extremen Bedingungen 2.17. ULLMANN, W.: Thermische Zustandsgleichung und GRÜNEISEN-Parameter zur Erforschung des tiefen Erdinneren 2.18. DITTFELD, H.-J.: Experimentelle Aussagen zum dynamischen Effekt des flüssigen Erdkerns 2.19. KOWALLE, G.: Untersuchung zur Dämpfung seismischer Wellen im Erdkern 2.20. DONNER, F. ; GÖTHE, W.; KNOTHE, C.; OELSNER, C.; PORSTENDORFER, G.:Beiträge der Tiefenelektromagnetik, Tiefenseismik und Geothermie zum Geodynamik-Projekt 2.21. HURTIG, E.; STROMEYER, D.: Temperatur-Tiefenverteilung und Viskosität im oberen Erdmantel unter Europa 2.22. OELSNER, C.: Eine Wärmestromanomalie im Gebiet von Freiberg (Sachsen) (in memorian Ferdinand Reich) 2.23. STROMEYER, D.: Studien zur Inversion geothermischer Daten 2.24. MAYER, P.: Einige Ergebnisse magnetisoher Messungen· im Nordatlantik 2.25. MENNING, M.: Tektonische Untersuchungen mit Hilfe der paläomagnetischen Bearbeitung von Bohrkernen 2.26. ROTHER, K.; WIEGANK, F.: Zur Interpretation paläomagnetischer Daten von Europa 2.27. MUNDT, W.: Zum Nachweis lokaler Säkularvariationsanomalien im Gebiet der DDR 2.28. MUNDT, W.; PORSTENDORFER, G.: Mögliche Zusammenhänge zwischen einer elektrischen Leitfähigkeitsanomalie im Erdmantel und anomalen magnetischen Säkularvariationen in Mitteleuropa 2.29. RITTER, E.: Zum Problem geoelektrischer Leitfähigkeitsanomalien und Tiefenbau von Kruste und oberem Mantel 2.30. HARWARDT, H.: Aufbau einer Strainmeteranlage in der Untertagestation Tiefenort 2.31. HARNISCH, G.: Zur Autokorrelationsfunktion der rezenten vertikalen Krustenbewegungen 2.32. THURM, H.; BANKWITZ, P.; HARNISCH, G.: Rezente horizontale Deformationen der Erdkruste im Südostteil der Deutschen Demokratischen Republik 2.33. KAUTZLEBEN, H.: Zur geophysikalischen Interpretation der planetaren Dynamik der Erde 3. Ergänzende Literatur 3.1. Untersuchung zur Geologie und Geophysik von Meeresböden (WG 4) 3.2. Rezente Erdkrustenbewegungen (WG 5) 3.3. Beziehungen zwischen Metamorphose und Tektonik (WG 9) 4. Autorenverzeichnis , Beiträge teilweise in deutscher, teilweise in englischer Sprache
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  • 66
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 9/G 9177
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 218 S. : graph. Darst.
    Series Statement: Developments in sedimentology 21
    Language: English
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  • 67
    Monograph available for loan
    Monograph available for loan
    Tulsa : Society of Exploration Geophysicists
    Associated volumes
    Call number: 5/M 93.1037
    In: Investigations in geophysics
    Type of Medium: Monograph available for loan
    Pages: xii, 526 S.
    ISBN: 0931830400
    Series Statement: Investigations in geophysics 2
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 68
    Monograph available for loan
    Monograph available for loan
    Washington, D.C. : Mineralogical Society of America
    Associated volumes
    Call number: 11/M 94.0162
    In: Reviews in mineralogy
    Description / Table of Contents: Geochemistry is a science that is based on an understanding of chemical processes in the earth. One of the principal tools available to the chemist for understanding systems at equilibrium is thermodynamics. The awareness and application of thermodynamic techniques has increased at a very fast pace in geosciences; in fact, one may be so bold as to say that thermodynamics in geology has reached the "mature" stage, although much future thermodynamic research is certainly needed. However, the natural processes in the earth are often sluggish enough that a particular system may not reach equilibrium. This observation is being supported constantly by new experimental and field data available to the geochemist e.g. the non-applicability of the phase rule in some assemblages, the compositional inhomogeneities of mineral grains, the partial reaction rims surrounding original minerals, the lack of isotopic equilibration or the absence of minerals (e.g. dolomite), which should be present according to thermodynamics. The need to apply kinetics has produced a large number of papers dealing with kinetics in geochemistry. As an initial response to this growing field, a conference on geochemical transport and kinetics was conducted at Airlie House, VA, in 1973, sponsored by the Carnegie Institution of Washington. The papers there dealt with several kinetic topics including diffusion, exsolution, metasomatism and metamorphic layering. Since 1973 the number of kinetic papers has continued to increase greatly. Therefore, the time is ripe for a Short Course in Kinetics, which brings together the fundamentals needed to explain field observations using kinetic data. It is hoped that this book may serve, not only as a reference for researchers dealing with the rates of geochemical processes, but also as a text in courses on geochemical kinetics. One of us has found this need of a text in teaching a graduate course on geochemical kinetics at Harvard and at Penn State during the past several years. Finally, it is our hope that the book may itself further even more research into the rates of geochemical processes and into the quantification of geochemical observations. The book is organized with a rough temperature gradient in mind, i.e. low temperature kinetics at the beginning and igneous kinetics at the end (no prejudices are intended with this scheme!). However, the topics in each chapter are general enough that they can be applied often to any geochemical domain: sedimentary, metamorphic or igneous. The theory of kinetics operates at two complementary levels: the phenomenological and the atomistic. The former relies on macroscopic variables (e.g. temperature or concentrations) to describe the rates of reactions or the rates of transport; the latter relates the rates to the basic forces operating between the particular atomic or molecular species of any system. This book deals with both descriptions of the kinetics of geochemical processes. Chapter one sets the framework for the phenomenological theory of reaction rates. If any geochemical reaction is to be described quantitatively, the rate law must be experimentally obtained in a kinetically sound manner and the reaction mechanism must be understood. This applies to heterogeneous fluid-rock reactions such as those occurring during metamorphism, hydrothermal alteration or weathering as well as to homogeneous reactions. Chapter 2 extends the theory to the global kinetics of geochemical cycles. This enables the kinetic concepts of stability and feedback to be applied to the cycling of elements in the many reservoirs of the earth. Chapter 3 applies the phenomenological treatment of chapter 1 to diagenesis and weathering. The rate of dissolution of minerals as well as the chemical evolution of pore waters are discussed. The atomistic basis of rates of reaction, transition state theory, is introduced in Chapter 4. Transition state theory can be applied to relate the rate constants of geochemical reactions to the atomic processes taking place. This includes not only homogeneous reactions but also reactions that occur at the surface of minerals. Chapter 5 discusses the theory of irreversible thermodynamics and its application to petrology. The use of the second law of thermodynamics along with the expressions for the rate of entropy production in a system have been used successfully since 1935 to describe kinetic phenomena. The chapter applies the concepts to the growth of minerals during metamorphism as well as to the formation of differentiated layers (banding) in petrology. Chapter 6 describes the phenomenological theory of diffusion both in aqueous solutions and in minerals. In particular, the multicomponent nature of diffusion and its consequence in natural systems is elaborated. Chapter 7 provides the atomistic basis for the rates of reactions in minerals. Understanding of the rates of diffusion, conduction, order-disorder reactions or exsolution in minerals depends on proper description of the defects in the various mineral structures. Chapter 8 provides the kinetic theory of crystal nucleation and growth. While many of the concepts in the chapter can be applied to aqueous systems, the emphasis is on igneous processes occurring during crystallization of a melt. To fully understand both the mineral composition as well as the texture of igneous rocks, the processes whereby new crystals form and grow must be quantified by using kinetic theory. Due to space and time limitations (kinetics!) some topics have not been covered in detail. In particular, the mathematical solution of diffusion or conduction equations is discussed very well by Crank in his book, Mathematics of Diffusion, and so is not covered to a great extent here. The treatment of fluid flow (e.g. convection) is also not covered in the text.
    Type of Medium: Monograph available for loan
    Pages: x, 398 S.
    ISBN: 0-939950-08-1 , 978-0-939950-08-9
    ISSN: 1529-6466
    Series Statement: Reviews in mineralogy 8
    Classification:
    Mineralogy
    Language: English
    Note: Chapter 1. Rate Laws of Chemical Reactions by Antonio C. Lasaga, p. 1 - 68 Chapter 2. Dynamic Treatment of Geochemical Cycles: Global Kinetics by Antonio C. Lasaga, p. 69 - 110 Chapter 3. Kinetics of Weathering and Diagenesis by Robert A. Berner, p. 111 - 134 Chapter 4. Transition State Theory by Antonio C. Lasaga, p. 135 - 170 Chapter 5. Irreversible Thermodynamics in Petrology by George W. Fisher and Antonio C. Lasaga, p. 171 - 210 Chapter 6. Diffusion in Electrolyte Mixtures by David E. Anderson, p. 211 - 260 Chapter 7. The Atomistic Basis of Kinetics: Defects in Minerals by Antonio C. Lasaga, p. 261 - 320 Chapter 8. Kinetics of Crystallization of Igneous Rocks by R. James Kirkpatrick, p. 321 - 398
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  • 69
    Call number: 9/M 92.0582
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: XII, 637 S. , Ill., graph. Darst., Kt.
    ISBN: 0632016051
    Series Statement: Geological Society special publication 28
    Classification:
    Tectonics
    Language: English
    Note: Paul Hancock: Appreciation: A. M. Quennell—a prescient tectonician / Geological Society, London, Special Publications, 28:x-xii, doi:10.1144/GSL.SP.1987.028.01.01 --- Fault Geometry and Associated Processes --- J. A. Jackson: Active normal faulting and crustal extension / Geological Society, London, Special Publications, 28:3-17, doi:10.1144/GSL.SP.1987.028.01.02 --- A. Gibbs: Development of extension and mixed-mode sedimentary basins / Geological Society, London, Special Publications, 28:19-33, doi:10.1144/GSL.SP.1987.028.01.03 --- N. J. Kusznir and R. G. Park: The extensional strength of the continental lithosphere: its dependence on geothermal gradient, and crustal composition and thickness / Geological Society, London, Special Publications, 28:35-52, doi:10.1144/GSL.SP.1987.028.01.04 --- H. David Lynch and Paul Morgan: The tensile strength of the lithosphere and the localization of extension / Geological Society, London, Special Publications, 28:53-65, doi:10.1144/GSL.SP.1987.028.01.05 --- C. E. Keen: Some important consequences of lithospheric extension / Geological Society, London, Special Publications, 28:67-73, doi:10.1144/GSL.SP.1987.028.01.06 --- David Barr: Lithospheric stretching, detached normal faulting and footwall uplift / Geological Society, London, Special Publications, 28:75-94, doi:10.1144/GSL.SP.1987.028.01.07 --- B. Vendeville, P. R. Cobbold, P. Davy, P. Choukroune, and J. P. Brun: Physical models of extensional tectonics at various scales / Geological Society, London, Special Publications, 28:95-107, doi:10.1144/GSL.SP.1987.028.01.08 --- K. R. McClay and P. G. Ellis: Analogue models of extensional fault geometries / Geological Society, London, Special Publications, 28:109-125, doi:10.1144/GSL.SP.1987.028.01.09 --- P. L. Hancock and T. G. Bevan: Brittle modes of foreland extension / Geological Society, London, Special Publications, 28:127-137, doi:10.1144/GSL.SP.1987.028.01.10 --- M. R. Leeder and R. L. Gawthorpe: Sedimentary models for extensional tilt-block/half-graben basins / Geological Society, London, Special Publications, 28:139-152, doi:10.1144/GSL.SP.1987.028.01.11 --- Extension in the Basin and Range Province and East Pacific Margin --- W. Hamilton: Crustal extension in the Basin and Range Province, southwestern United States / Geological Society, London, Special Publications, 28:155-176, doi:10.1144/GSL.SP.1987.028.01.12 --- P. J. Coney: The regional tectonic setting and possible causes of Cenozoic extension in the North American Cordillera / Geological Society, London, Special Publications, 28:177-186, doi:10.1144/GSL.SP.1987.028.01.13 --- L. J. Sonder, P. C. England, B. P. Wernicke, and R. L. Christiansen: A physical model for Cenozoic extension of western North America / Geological Society, London, Special Publications, 28:187-201, doi:10.1144/GSL.SP.1987.028.01.14 --- Brian P. Wernicke, Philip C. England, Leslie J. Sonder, and Robert L. Christiansen: Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera / Geological Society, London, Special Publications, 28:203-221, doi:10.1144/GSL.SP.1987.028.01.15 --- Richard W. Allmendinger, Jack Oliver, Thomas A. Hauge, Ernest C. Hauser, and Christopher J. Potter: Tectonic heredity and the layered lower crust in the Basin and Range Province, western United States / Geological Society, London, Special Publications, 28:223-246, doi:10.1144/GSL.SP.1987.028.01.16 --- George H. Davis: A shear-zone model for the structural evolution of metamorphic core complexes in southeastern Arizona / Geological Society, London, Special Publications, 28:247-266, doi:10.1144/GSL.SP.1987.028.01.17 --- Jeffrey Lee, Elizabeth L. Miller, and John F. Sutter: Ductile strain and metamorphism in an extensional tectonic setting: a case study from the northern Snake Range, Nevada, USA / Geological Society, London, Special Publications, 28:267-298, doi:10.1144/GSL.SP.1987.028.01.18 --- Keith A. Howard and Barbara E. John: Crustal extension along a rooted system of imbricate low-angle faults: Colorado River extensional corridor, California and Arizona / Geological Society, London, Special Publications, 28:299-311, doi:10.1144/GSL.SP.1987.028.01.19 --- Barbara E. John: Geometry and evolution of a mid-crustal extensional fault system: Chemehuevi Mountains, southeastern California / Geological Society, London, Special Publications, 28:313-335, doi:10.1144/GSL.SP.1987.028.01.20 --- Ronald L. Bruhn, Pamela R. Gibler, and William T. Parry: Rupture characteristics of normal faults: an example from the Wasatch fault zone, Utah / Geological Society, London, Special Publications, 28:337-353, doi:10.1144/GSL.SP.1987.028.01.21 --- Gordon P. Eaton: Topography and origin of the southern Rocky Mountains and Alvarado Ridge / Geological Society, London, Special Publications, 28:355-369, doi:10.1144/GSL.SP.1987.028.01.22 --- Paul K. Eddington, Robert B. Smith, and C. Renggli: Kinematics of Basin and Range intraplate extension / Geological Society, London, Special Publications, 28:371-392, doi:10.1144/GSL.SP.1987.028.01.23 --- K. V. Hodges, J. D. Walker, and B. P. Wernicke: Footwall structural evolution of the Tucki Mountain detachment system, Death Valley region, southeastern California / Geological Society, London, Special Publications, 28:393-408, doi:10.1144/GSL.SP.1987.028.01.24 --- Bob Thompson, Eric Mercier, and Charlie Roots: Extension and its influence on Canadian Cordilleran passive-margin evolution / Geological Society, London, Special Publications, 28:409-417, doi:10.1144/GSL.SP.1987.028.01.25 --- S. W. Garrett and B. C. Storey: Lithospheric extension on the Antarctic Peninsula during Cenozoic subduction / Geological Society, London, Special Publications, 28:419-431, doi:10.1144/GSL.SP.1987.028.01.26 --- I. W. D. Dalziel, A. M. Grunow, B. C. Storey, S. W. Garrett, L. D. B. Herrod, and R. J. Pankhurst: Extensional tectonics and the fragmentation of Gondwanaland / Geological Society, London, Special Publications, 28:433-441, doi:10.1144/GSL.SP.1987.028.01.27 --- Extension in the NW European Continental Shelf --- M. J. Cheadle, S. McGeary, M. R. Warner, and D. H. Matthews: Extensional structures on the western UK continental shelf: a review of evidence from deep seismic profiling / Geological Society, London, Special Publications, 28:445-465, doi:10.1144/GSL.SP.1987.028.01.28 --- Alastair Beach, Tim Bird, and Alan Gibbs: Extensional tectonics and crustal structure: deep seismic reflection data from the northern North Sea Viking graben / Geological Society, London, Special Publications, 28:467-476, doi:10.1144/GSL.SP.1987.028.01.29 --- F. Zervos: A compilation and regional interpretation of the northern North Sea gravity map / Geological Society, London, Special Publications, 28:477-493, doi:10.1144/GSL.SP.1987.028.01.30 --- Stephen E. Laubach and Stephen Marshak: Fault patterns generated during extensional deformation of crystalline basement, NW Scotland / Geological Society, London, Special Publications, 28:495-499, doi:10.1144/GSL.SP.1987.028.01.31 --- S. R. Kirton and K. Hitchen: Timing and style of crustal extension N of the Scottish mainland / Geological Society, London, Special Publications, 28:501-510, doi:10.1144/GSL.SP.1987.028.01.32 --- C. R. Fielding and G. A. L. Johnson: Sedimentary structures associated with extensional fault movement from the Westphalian of NE England / Geological Society, London, Special Publications, 28:511-516, doi:10.1144/GSL.SP.1987.028.01.33 --- Garry D. Karner, Stuart D. Lake, and John F. Dewey: The thermal and mechanical development of the Wessex Basin, southern England / Geological Society, London, Special Publications, 28:517-536, doi:10.1144/GSL.SP.1987.028.01.34 --- Michel Seranne and Michel Seguret: The Devonian basins of western Norway: tectonics and kinematics of an extending crust / Geological Society, London, Special Publications, 28:537-548, doi:10.1144/GSL.SP.1987.028.01.35 --- Extension in the Middle Eas
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  • 70
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 15/M 92.0485
    In: Developments in geotechnical engineering
    Type of Medium: Monograph available for loan
    Pages: 621 S.
    ISBN: 0444989560
    Series Statement: Developments in geotechnical engineering 44
    Classification:
    Seismology
    Language: English
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  • 71
    Monograph available for loan
    Monograph available for loan
    Alexandria : American Geological Inst.
    Call number: M 94.0103 ; 1.2/WE 85
    Type of Medium: Monograph available for loan
    Pages: X, 788 S.
    Edition: 3rd. ed.
    ISBN: 0913312894
    Classification:
    E.5.
    Language: English
    Location: Upper compact magazine
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  • 72
    Call number: MOP 44887 / Regal 13 ; MOP 44887/A / Mitte ; MOP 43468 / Mitte
    In: Studies and reports in hydrology
    Description / Table of Contents: This monograph shows the results of studies of the laws of water circulation and the water balance of the world. Data on water storage of the earth are given as well as on the areal distribution of water resources and periods of natural recharge of some types of water resources. Computations are presented of the water balance of large river basins, lakes, reservoirs, regions, continents, oceans and the whole globe. Fresh-water resources of the world and their time and space variations are evaluated. On the basis of new data, including areas whose hydrometeorological factors have been poorly gauged, the "Atlas of World Water Balance" was prepared to accompany the monograph. All maps published are original. The monograph is intended for specialists engaged in water-balance computations and water resources development and conservation.
    Type of Medium: Monograph available for loan
    Pages: 663 S. : graph. Darst., Kt.
    ISBN: 9231014978
    Series Statement: Studies and reports in hydrology 25
    Uniform Title: Mirovoj vodnyi balans i vodnye resursy zmeli 〈engl.〉
    Language: English
    Location: Reading room
    Location: MOP - must be ordered
    Location: MOP - must be ordered
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  • 73
    Series available for loan
    Series available for loan
    Potsdam : Zentralinstitut Physik der Erde
    Associated volumes
    Call number: 21/SR 90.0917(89) ; 21/SR 22.19544(89)
    In: Veröffentlichungen des Zentralinstituts Physik der Erde, Nr. 89
    In: Geodetic boundary value problems, II
    Type of Medium: Series available for loan
    Pages: 229 Seiten , Illustrationen , 30 cm
    Edition: Als Manuskript gedruckt
    ISSN: 0514-8790
    Series Statement: Veröffentlichungen des Zentralinstituts Physik der Erde Nr. 89
    Language: English
    Note: A. A test for the Marussi condition. B. On the evaluation of the numerical amount of the residual term of the solution of the geodetic boundary value problem. C. The solution of the first mixed boundary value problem of the geodesy as an optimal method for the computation of the altimetrygravimetry problem. D. Gravity disturbances as boundary values on the surface of the Earth. E. A proof of the convergence of the spherical - harmonics series development of a potential exterior of a regular surface by the completeness of the system of the base functions at the surface.
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  • 74
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell
    Associated volumes
    Call number: 9/M 92.1245 ; M 93.0059/33
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: X, 575 S. , Ill., zahlr. graph. Darst., Kt.
    ISBN: 0632018062
    Series Statement: Geological Society special publication 33
    Classification:
    Petrology, Petrography
    Language: English
    Note: General Topics and Reviews --- S. R. Taylor: Geochemical and Petrological Significance of the Archaean-Proterozoic Boundary / Geological Society, London, Special Publications, 33:3-8, doi:10.1144/GSL.SP.1987.033.01.01 --- R. P. Hall, D. J. Hughes, C. R. L. Friend, and G. L. Snyder: Proterozoic Mantle Heterogeneity: Geochemical Evidence from Contrasting Basic Dykes / Geological Society, London, Special Publications, 33:9-21, doi:10.1144/GSL.SP.1987.033.01.02 --- D. Rickard: Proterozoic Volcanogenic Mineralization Styles / Geological Society, London, Special Publications, 33:23-35, doi:10.1144/GSL.SP.1987.033.01.03 --- Early Proterozoic Volcanic Suites of the Baltic Shield --- T. C. Pharaoh, A. Warren, and N. J. Walsh: Early Proterozoic Metavolcanic Suites of the Northernmost Part of the Baltic Shield / Geological Society, London, Special Publications, 33:41-58, doi:10.1144/GSL.SP.1987.033.01.04 --- M. Honkamo: Geochemistry and Tectonic Setting of Early Proterozoic Volcanic Rocks in Northern Ostrobothnia, Finland / Geological Society, London, Special Publications, 33:59-68, doi:10.1144/GSL.SP.1987.033.01.05 --- Waldo Vivallo and Lars-Åke Claesson: Intra-Arc Rifting and Massive Sulphide Mineralization in an Early Proterozoic Volcanic Arc, Skellefte District, Northern Sweden / Geological Society, London, Special Publications, 33:69-79, doi:10.1144/GSL.SP.1987.033.01.06 --- Joanna Parr and David Rickard: Early Proterozoic Subaerial Volcanism and Its Relationship to Broken Hill-type Mineralization in Central Sweden / Geological Society, London, Special Publications, 33:81-93, doi:10.1144/GSL.SP.1987.033.01.07 --- H. Colley and L. Westra: The Volcano-Tectonic Setting and Mineralization of the Early Proterozoic Kemiö-Orijärvi-Lohja Belt, SW Finland / Geological Society, London, Special Publications, 33:95-107, doi:10.1144/GSL.SP.1987.033.01.08 --- Early and Middle Proterozoic Volcanic Suites of the Laurentian and North Atlantic Shields --- W. R. A. Baragar and R. F. J. Scoates: Volcanic Geochemistry of the Northern Segments of the Circum-Superior Belt of the Canadian Shield / Geological Society, London, Special Publications, 33:113-131, doi:10.1144/GSL.SP.1987.033.01.09 --- N. T. Arndt, G. E. Brügmann, K. Lehnert, C. Chauvel, and B. W. Chappell: Geochemistry, Petrogenesis and Tectonic Environment of Circum-Superior Belt Basalts, Canada / Geological Society, London, Special Publications, 33:133-145, doi:10.1144/GSL.SP.1987.033.01.10 --- J. F. Lewry, R. MacDonald, C. Livesey, M. Meyer, R. Van Schmus, and M. E. Bickford: U-Pb Geochronology of Accreted Terranes in the Trans-Hudson Orogen, Northern Saskatchewan, Canada / Geological Society, London, Special Publications, 33:147-166, doi:10.1144/GSL.SP.1987.033.01.11 --- B. R. Watters and J. A. Pearce: Metavolcanic Rocks of the La Ronge Domain in the Churchill Province, Saskatchewan: Geochemical Evidence for a Volcanic Arc Origin / Geological Society, London, Special Publications, 33:167-182, doi:10.1144/GSL.SP.1987.033.01.12 --- J. W. Gaskarth and G. R. Parslow: Proterozoic Volcanism in the Flin Flon Greenstone Belt, East-Central Saskatchewan, Canada / Geological Society, London, Special Publications, 33:183-200, doi:10.1144/GSL.SP.1987.033.01.13 --- Charles F. Gower and Bruce Ryan: Two Stage Felsic Volcanism in the Lower Proterozoic Upper Aillik Group, Labrador, Canada: Its Relationship to Syn- and Post-Kinematic Plutonism / Geological Society, London, Special Publications, 33:201-210, doi:10.1144/GSL.SP.1987.033.01.14 --- K. C. Condie: Early Proterozoic Volcanic Regimes in Southwestern North America / Geological Society, London, Special Publications, 33:211-218, doi:10.1144/GSL.SP.1987.033.01.15 --- A. N. LeCheminant, A. R. Miller, and G. M. LeCheminant: Early Proterozoic Alkaline Igneous Rocks, District of Keewatin, Canada: Petrogenesis and Mineralization / Geological Society, London, Special Publications, 33:219-240, doi:10.1144/GSL.SP.1987.033.01.16 --- A. B. Ryan, W. R. A. Baragar, and D. J. Kontak: Geochemistry, Tectonic Setting, and Mineralization of High-Potassium Middle Proterozoic Rocks in Central Labrador, Canada / Geological Society, London, Special Publications, 33:241-254, doi:10.1144/GSL.SP.1987.033.01.17 --- Y. A. Johnson, R. G. Park, and J. A. Winchester: Geochemistry, Petrogenesis and Tectonic Significance of the Early Proterozoic Loch Maree Group Amphibolites of the Lewisian Complex, NW Scotland / Geological Society, London, Special Publications, 33:255-269, doi:10.1144/GSL.SP.1987.033.01.18 --- Proterozoic Volcanic Suites of the Guiana Shield --- A. K. Gibbs: Proterozoic Volcanic Rocks of the Northern Guiana Shield, South America / Geological Society, London, Special Publications, 33:275-288, doi:10.1144/GSL.SP.1987.033.01.19 --- R. Renner and A. K. Gibbs: Geochemistry and Petrology of Metavolcanic Rocks of the Early Proterozoic Mazaruni Greenstone Belt, Northern Guyana / Geological Society, London, Special Publications, 33:289-309, doi:10.1144/GSL.SP.1987.033.01.20 --- Proterozoic Volcanic Suites of Africa --- R. E. Myers, R. G. Cawthorn, T. S. McCarthy, and C. R. Anhaeusser: Fundamental Uniformity in the Trace Element Patterns of the Volcanics of the Kaapvaal Craton from 3000 to 2100 Ma: Evidence for the Lithospheric Origin of These Continental Tholeiites / Geological Society, London, Special Publications, 33:315-325, doi:10.1144/GSL.SP.1987.033.01.21 --- D. L. Reid, A. J. Erlank, H. J. Welke, and A. Moyes: The Orange River Group: a Major Proterozoic Calcalkaline Volcanic Belt in the Western Namaqua Province, Southern Africa / Geological Society, London, Special Publications, 33:327-346, doi:10.1144/GSL.SP.1987.033.01.22 --- G. Borg and K. J. Maiden: Alteration of Late Middle Proterozoic Volcanics and its Relation to Stratabound Copper-Silver-Gold Mineralization Along the Margin of the Kalahari Craton in Swa/Namibia and Botswana / Geological Society, London, Special Publications, 33:347-354, doi:10.1144/GSL.SP.1987.033.01.23 --- J. H. Breitkopf and K. J. Maiden: Geochemical Patterns of Metabasites in the Southern Part of the Damara Orogen, SWA/Namibia: Applicability to the Recognition of Tectonic Environment / Geological Society, London, Special Publications, 33:355-361, doi:10.1144/GSL.SP.1987.033.01.24 --- P. M. Klemenic: The Geochemistry of Upper Proterozoic Lavas From the Red Sea Hills, NE Sudan / Geological Society, London, Special Publications, 33:363-372, doi:10.1144/GSL.SP.1987.033.01.25 --- Proterozoic Volcanic Suites of Australia --- L. A. I. Wyborn, R. W. Page, and A. J. Parker: Geochemical and Geochronological Signatures in Australian Proterozoic Igneous Rocks / Geological Society, London, Special Publications, 33:377-394, doi:10.1144/GSL.SP.1987.033.01.26 --- S. D. James, J. A. Pearce, and R. A. Oliver: The Geochemistry of the Lower Proterozoic Willyama Complex Volcanics, Broken Hill Block, New South Wales / Geological Society, London, Special Publications, 33:395-408, doi:10.1144/GSL.SP.1987.033.01.27 --- I. H. Wilson: Geochemistry of Proterozoic Volcanics, Mount Isa Inlier, Australia / Geological Society, London, Special Publications, 33:409-423, doi:10.1144/GSL.SP.1987.033.01.28 --- L. A. I. Wyborn: The Petrology and Geochemistry of Alteration Assemblages in the Eastern Creek Volcanics, as a Guide to Copper and Uranium Mobility Associated with Regional Metamorphism and Deformation, Mount Isa, Queensland / Geological Society, London, Special Publications, 33:425-434, doi:10.1144/GSL.SP.1987.033.01.29 --- Proterozoic Volcanic Suites of Asia --- Jia Chengzao: Geochemistry and Tectonics of the Xionger Group in the Eastern Qinling Mountains of China—a mid Proterozoic Volcanic arc Related to Plate Subduction / Geological Society, London, Special Publications, 33:436-448, doi:10.1144/GSL.SP.1987.033.01.30 --- Middle to Late Proterozoic Volcanic Suites of the North Atlantic Borderlands --- T. E. Smith and P. E. Holm: The Trace Element Geochemist
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    Chichester : Wiley
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    Call number: 19/M 92.1225/6A
    In: Handbook of applicable mathematics
    Type of Medium: Monograph available for loan
    Pages: xxi, 498 S.
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  • 76
    Call number: 4/M 93.0760 ; M 92.0247
    In: Lecture notes in earth sciences
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    Pages: 393 S.
    ISBN: 3540182195
    Series Statement: Lecture notes in earth sciences 12
    Classification:
    Geodetic Theory and Modeling
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    New York [u.a.] : Wiley
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    Call number: 17/G 9062/2
    In: Inductively coupled plasma emission spectroscopy
    Type of Medium: Monograph available for loan
    Pages: XII, 486 S.
    ISBN: 047185378X
    Series Statement: 90,2
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  • 78
    Call number: 9/M 92.0488
    In: Developments in volcanology
    Type of Medium: Monograph available for loan
    Pages: VII, 652 S.
    ISBN: 044442234x
    Series Statement: Developments in volcanology 2
    Classification:
    Petrology, Petrography
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    Washington, DC : American Geophysical Union [u.a.]
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    Call number: 4/M 92.1327/11
    In: Geodynamics series
    Type of Medium: Monograph available for loan
    Pages: 457 S.
    ISBN: 0875905005
    Series Statement: Geodynamics series 11
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    Geodynamics
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    New York : Wiley-Interscience
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    Call number: 19/M 92.1225/6B
    In: Handbook of applicable mathematics
    Type of Medium: Monograph available for loan
    Pages: S. 499-942, XXXVI, A43 S.
    Edition: Reprint.
    ISBN: 0471902721
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    C.1.1.
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  • 81
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    Oxford [u.a.] : Blackwell
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    Call number: 9/M 92.1248
    In: Geological Society special publication
    Description / Table of Contents: Alkaline igneous rocks may be defined as those which have higher concentrations of alkalis than can be accommodated in feldspars alone, the excess appearing as feldspathoids, sodic pyroxenes, sodic amphiboles and other alkali-rich phases. These rocks are, therefore, deficient in silica and/or alumina with respect to alkalis and will have nepheline and/or acmite in their norms. In practice the term ‘alkaline’ is used to encompass a wide range of igneous rocks, not all of which conform to this rigid definition. Carbonatites, for example, are certainly silica-deficient but are rarely alkali-rich. True (nepheline-normative) alkali basalts grade into hypersthene-normative transitional basalts without any obvious change in mineralogy. Since transitional basalts are often closely associated with alkali basalts in the field, they are traditionally regarded as alkaline. It is now usual practice to define alkaline igneous rocks simply in terms of their alkali (Na2O + K2O) and silica contents (see, for example, Le Bas et al. 1986). We have not attempted to review the classification of alkaline igneous rocks in this volume as this has been dealt with elsewhere (e.g. Sørensen 1974; Streckeisen 1967, 1980). The only alkaline rocks not covered in previous reviews are those hydrous mafic to ultramafic hypabyssal rocks known as the lamprophyres. The present volume includes three papers on this group. A comprehensive overview of lamprophyres is given by Rock and of the sub-group of lamproites by Bergman. The relationship between lamproites and kimberlites (which arguably belong to the lamprophyres) is discussed by Dawson.
    Type of Medium: Monograph available for loan
    Pages: XIV, 568 S. , Ill., graph. Darst., Kt.
    ISBN: 0632016167
    Series Statement: Geological Society special publication 30
    Classification:
    Petrology, Petrography
    Language: English
    Note: J. G. Fitton and B. G. J. Upton: Introduction / Geological Society, London, Special Publications, 30:ix-xiv, doi:10.1144/GSL.SP.1987.030.01.01 --- D. K. Bailey: Mantle metasomatism—perspective and prospect / Geological Society, London, Special Publications, 30:1-13, doi:10.1144/GSL.SP.1987.030.01.02 --- Martin Menzies: Alkaline rocks and their inclusions: a window on the Earth’s interior / Geological Society, London, Special Publications, 30:15-27, doi:10.1144/GSL.SP.1987.030.01.03 --- A. D. Edgar: The genesis of alkaline magmas with emphasis on their source regions: inferences from experimental studies / Geological Society, London, Special Publications, 30:29-52, doi:10.1144/GSL.SP.1987.030.01.04 --- M. J. Le Bas: Nephelinites and carbonatites / Geological Society, London, Special Publications, 30:53-83, doi:10.1144/GSL.SP.1987.030.01.05 --- James D. Twyman and John Gittins: Alkalic carbonatite magmas: parental or derivative? / Geological Society, London, Special Publications, 30:85-94, doi:10.1144/GSL.SP.1987.030.01.06 --- J. B. Dawson: The kimberlite clan: relationship with olivine and leucite lamproites, and inferences for upper-mantle metasomatism / Geological Society, London, Special Publications, 30:95-101, doi:10.1144/GSL.SP.1987.030.01.07 --- Steven C. Bergman: Lamproites and other potassium-rich igneous rocks: a review of their occurrence, mineralogy and geochemistry / Geological Society, London, Special Publications, 30:103-190, doi:10.1144/GSL.SP.1987.030.01.08 --- Nicholas M.S. Rock: The nature and origin of lamprophyres: an overview / Geological Society, London, Special Publications, 30:191-226, doi:10.1144/GSL.SP.1987.030.01.09 --- David A. Clague: Hawaiian alkaline volcanism / Geological Society, London, Special Publications, 30:227-252, doi:10.1144/GSL.SP.1987.030.01.10 --- Barry L. Weaver, David A. Wood, John Tarney, and Jean Louis Joron: Geochemistry of ocean island basalts from the South Atlantic: Ascension, Bouvet, St. Helena, Gough and Tristan da Cunha / Geological Society, London, Special Publications, 30:253-267, doi:10.1144/GSL.SP.1987.030.01.11 --- Chris Harris and Simon M.F. Sheppard: Magma and fluid evolution in the lavas and associated granite xenoliths of Ascension Island / Geological Society, London, Special Publications, 30:269-272, doi:10.1144/GSL.SP.1987.030.01.12 --- J. G. Fitton: The Cameroon line, West Africa: a comparison between oceanic and continental alkaline volcanism / Geological Society, London, Special Publications, 30:273-291, doi:10.1144/GSL.SP.1987.030.01.13 --- B.H. Baker: Outline of the petrology of the Kenya rift alkaline province / Geological Society, London, Special Publications, 30:293-311, doi:10.1144/GSL.SP.1987.030.01.14 --- R. Macdonald: Quaternary peralkaline silicic rocks and caldera volcanoes of Kenya / Geological Society, London, Special Publications, 30:313-333, doi:10.1144/GSL.SP.1987.030.01.15 --- A. R. Woolley and G. C. Jones: The petrochemistry of the northern part of the Chilwa alkaline province, Malawi / Geological Society, London, Special Publications, 30:335-355, doi:10.1144/GSL.SP.1987.030.01.16 --- P. Bowden, R. Black, R. F. Martin, E. C. Ike, J. A. Kinnaird, and R. A. Batchelor: Niger-Nigerian alkaline ring complexes: a classic example of African Phanerozoic anorogenic mid-plate magmatism / Geological Society, London, Special Publications, 30:357-379, doi:10.1144/GSL.SP.1987.030.01.17 --- J. P. Liégeois and R. Black: Alkaline magmatism subsequent to collision in the Pan-African belt of the Adrar des Iforas (Mali) / Geological Society, London, Special Publications, 30:381-401, doi:10.1144/GSL.SP.1987.030.01.18 --- C. J. N. Fletcher and B. Beddoe-Stephens: The petrology, chemistry and crystallization history of the Velasco alkaline province, eastern Bolivia / Geological Society, London, Special Publications, 30:403-413, doi:10.1144/GSL.SP.1987.030.01.19 --- Daniel S. Barker: Tertiary alkaline magmatism in Trans-Pecos Texas / Geological Society, London, Special Publications, 30:415-431, doi:10.1144/GSL.SP.1987.030.01.20 --- G. Nelson Eby: The Monteregian Hills and White Mountain alkaline igneous provinces, eastern North America / Geological Society, London, Special Publications, 30:433-447, doi:10.1144/GSL.SP.1987.030.01.21 --- B.G.J. Upton and C.H. Emeleus: Mid-Proterozoic alkaline magmatism in southern Greenland: the Gardar province / Geological Society, London, Special Publications, 30:449-471, doi:10.1144/GSL.SP.1987.030.01.22 --- Lotte Melchior Larsen and Henning Sørensen: The Ilímaussaq intrusion—progressive crystallization and formation of layering in an agpaitic magma / Geological Society, London, Special Publications, 30:473-488, doi:10.1144/GSL.SP.1987.030.01.23 --- T. F. D. Nielsen: Tertiary alkaline magmatism in East Greenland: a review / Geological Society, London, Special Publications, 30:489-515, doi:10.1144/GSL.SP.1987.030.01.24 --- Hilary Downes: Tertiary and Quaternary volcanism in the Massif Central, France / Geological Society, London, Special Publications, 30:517-530, doi:10.1144/GSL.SP.1987.030.01.25 --- L. N. Kogarko: Alkaline rocks of the eastern part of the Baltic Shield (Kola Peninsula) / Geological Society, London, Special Publications, 30:531-544, doi:10.1144/GSL.SP.1987.030.01.26
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    Monograph available for loan
    Oxford [u.a.] : Blackwell
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    Call number: 9/M 93.0662
    In: Geological Society special publication
    Description / Table of Contents: Tropical deserts have existed sporodically on our planet from the Precambrian to the Present, and seem not to have been a permanent feature of its surface (Glennie 1987). Depending on their definition, tropical deserts and semi-deserts currently occupy between approximately one fifth and one third of the Earth’s land surface, of which only about 4% is covered by that popular concept of what a desert consists of—sand dunes. The remaining area comprises barren rock (both hill and plateau) with a variable cover of sediments transported by ephemeral streams (wadis, arroyos) to form the deposits at the terminal points of these streams. Varying with the ratio of water supply to the annual potential rate of evaporation, those terminal areas may be occupied by desert lakes that are generally of a temporary nature (permanent only if the water is provided from beyond the margins of the desert or is fed by groundwater), and become more saline as they become desiccated. The end product of such a situation is a salina or sabkha (area of sand, silt or clay, commonly encrusted with halite). There is no universally accepted definition of a desert. In its simplest form it can be defined as a barren tract of land over which rainfall is too limited or spasmodic to support vegetation adequately. Very few desert areas are completely devoid of vegetation, and many areas that fall within a desert in terms of average annual rainfall may have an even though sparse cover of plants that have adapted to the relatively arid environment in which they live. In this context, some writers define deserts as areas that have an average upper limit of 250 mm of annual rainfall, even though it may all fall in one storm and rainfall may not recur for several years. Perhaps more important than the rainfall itself is the ratio between it and the potential rate of evaporation—the aridity or desiccation factor. This is about 1:10 in some parts of the Australian Desert and up to 1:500 in areas of the Sahara (Cooke & Warren 1973).
    Type of Medium: Monograph available for loan
    Pages: XI, 401 S. , zahlr. Ill. u graph. Darst.
    ISBN: 0632019050
    Series Statement: Geological Society special publication 35
    Classification:
    Petrology, Petrography
    Language: English
    Note: Introduction --- K. W. Glennie: Desert sediments: ancient and modern / Geological Society, London, Special Publications, 35:1-4, doi:10.1144/GSL.SP.1987.035.01.01: Fluvial Sediments: Process and Form --- A. P. Schick, J. Lekach, and M. A. Hassan: Vertical exchange of coarse bedload in desert streams / Geological Society, London, Special Publications, 35:7-16, doi:10.1144/GSL.SP.1987.035.01.02 --- S. Grossman and R. Gerson: Fluviatile deposits and morphology of alluvial surfaces as indicators of Quaternary environmental changes in the southern Negev, Israel / Geological Society, London, Special Publications, 35:17-29, doi:10.1144/GSL.SP.1987.035.01.03 --- J. K. Maizels: Plio-Pleistocene raised channel systems of the western Sharqiya (Wahiba), Oman / Geological Society, London, Special Publications, 35:31-50, doi:10.1144/GSL.SP.1987.035.01.04 --- Tectonism, Climatic Change and Fluviatile Desert Sediments --- L. E. Frostick and I. Reid: Tectonic control of desert sediments in rift basins ancient and modern / Geological Society, London, Special Publications, 35:53-68, doi:10.1144/GSL.SP.1987.035.01.05 --- H. Olsen: Ancient ephemeral stream deposits: a local terminal fan model from the Bunter Sandstone Formation (L. Triassic) in the Tønder-3, -4 and -5 wells, Denmark / Geological Society, London, Special Publications, 35:69-86, doi:10.1144/GSL.SP.1987.035.01.06 --- A. M. Harvey: Alluvial fan dissection: relationships between morphology and sedimentation / Geological Society, London, Special Publications, 35:87-103, doi:10.1144/GSL.SP.1987.035.01.07 --- M. A. J. Williams, P. I. Abell, and B. W. Sparks: Quaternary landforms, sediments, depositional environments and gastropod isotope ratios at Adrar Bous, Tenere Desert of Niger, south-central Sahara / Geological Society, London, Special Publications, 35:105-125, doi:10.1144/GSL.SP.1987.035.01.08 --- Aeolian Sediments: Dust Dynamics and Deposits --- W. B. Whalley, B. J. Smith, J. J. McAlister, and A. J. Edwards: Aeolian abrasion of quartz particles and the production of silt-size fragments: preliminary results / Geological Society, London, Special Publications, 35:129-138, doi:10.1144/GSL.SP.1987.035.01.09 --- K. Pye and H. Tsoar: The mechanics and geological implications of dust transport and deposition in deserts with particular reference to loess formation and dune sand diagenesis in the northern Negev, Israel / Geological Society, London, Special Publications, 35:139-156, doi:10.1144/GSL.SP.1987.035.01.10 --- R. Gerson and R. Amit: Rates and modes of dust accretion and deposition in an arid region—the Negev, Israel / Geological Society, London, Special Publications, 35:157-169, doi:10.1144/GSL.SP.1987.035.01.11 --- H. Vine: Wind-blown materials and W African soils: an explanation of the ‘ferrallitic soil over loose sandy sediments’ profile / Geological Society, London, Special Publications, 35:171-183, doi:10.1144/GSL.SP.1987.035.01.12 --- Dune Dynamics and Deposits --- A. Gunatilaka and S. Mwango: Continental sabkha pans and associated nebkhas in southern Kuwait, Arabian Gulf / Geological Society, London, Special Publications, 35:187-203, doi:10.1144/GSL.SP.1987.035.01.13 --- A. Warren and S. Kay: Dune networks / Geological Society, London, Special Publications, 35:205-212, doi:10.1144/GSL.SP.1987.035.01.14 --- L. B. Clemmensen: Complex star dunes and associated aeolian bedforms, Hopeman Sandstone (Permo-Triassic), Moray Firth Basin, Scotland / Geological Society, London, Special Publications, 35:213-231, doi:10.1144/GSL.SP.1987.035.01.15 --- B. P. J. Williams, E. K. Wild, and R. J. Suttill: Late Palaeozoic cold-climate aeolianites, southern Cooper Basin, South Australia / Geological Society, London, Special Publications, 35:233-249, doi:10.1144/GSL.SP.1987.035.01.16 --- R. A. Carruthers: Aeolian sedimentation from the Galtymore Formation (Devonian), Ireland / Geological Society, London, Special Publications, 35:251-268, doi:10.1144/GSL.SP.1987.035.01.17 --- Grain Size, Process and Dune Environment --- E. C. Flenley, N. R. J. Fieller, and D. D. Gilbertson: The statistical analysis of ‘mixed’ grain size distributions from aeolian sands in the Libyan Pre-Desert using log skew Laplace models / Geological Society, London, Special Publications, 35:271-280, doi:10.1144/GSL.SP.1987.035.01.18 --- I. Livingstone: Grain-size variation on a ‘complex’ linear dune in the Namib Desert / Geological Society, London, Special Publications, 35:281-291, doi:10.1144/GSL.SP.1987.035.01.19 --- D. S. G. Thomas: Discrimination of depositional environments using sedimentary characteristics in the Mega Kalahari, central southern Africa / Geological Society, London, Special Publications, 35:293-306, doi:10.1144/GSL.SP.1987.035.01.20 --- Chemical Sediments --- D. A. Hendry: Silica and calcium carbonate replacement of plant roots in tropical dune sands, SE India / Geological Society, London, Special Publications, 35:309-319, doi:10.1144/GSL.SP.1987.035.01.21 --- C. R. Roberts and C. W. Mitchell: Spring mounds in southern Tunisia / Geological Society, London, Special Publications, 35:321-334, doi:10.1144/GSL.SP.1987.035.01.22 --- Remote Sensing of Desert Sediments --- C. S. Breed, J. F. McCauley, and P. A. Davis: Sand sheets of the eastern Sahara and ripple blankets on Mars / Geological Society, London, Special Publications, 35:337-359, doi:10.1144/GSL.SP.1987.035.01.23 --- M. M. Ashour: Surficial deposits of Qatar Peninsula / Geological Society, London, Special Publications, 35:361-367, doi:10.1144/GSL.SP.1987.035.01.24 --- A. C. Millington, A. R. Jones, N. Quarmby, and J. R. G. Townshend: Remote sensing of sediment transfer processes in playa basins / Geological Society, London, Special Publications, 35:369-381, doi:10.1144/GSL.SP.1987.035.01.25
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    Monograph available for loan
    New York [u.a.] : Wiley
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    Call number: 17/G 9062/1
    In: Inductively coupled plasma emission spectroscopy
    Type of Medium: Monograph available for loan
    Pages: XI, 584 S.
    ISBN: 0471096865
    Series Statement: 90,1
    Language: English
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    Associated volumes
    Call number: 5/G 8861/1
    In: Geomagnetism
    Type of Medium: Monograph available for loan
    Pages: xvii, 627 S.
    ISBN: 0123786711
    Classification:
    Geomagnetism, Geoelectromagnetism
    Language: English
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  • 85
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    Monograph available for loan
    Washington : American Geophysical Union
    Associated volumes
    Call number: 4/M 92.1327/9
    In: Geodynamics series
    Type of Medium: Monograph available for loan
    Pages: 170 S.
    ISBN: 0875905021
    Series Statement: Geodynamics series 9
    Language: English
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  • 86
    Monograph available for loan
    Monograph available for loan
    London [u.a.] : Geophysical Press
    Associated volumes
    Call number: 5/M 92.1088
    In: Handbook of geophysical exploration
    Type of Medium: Monograph available for loan
    Pages: X, 568 S.
    ISBN: 0946631204
    Series Statement: Handbook of geophysical exploration : seismic exploration 20
    Classification:
    Geophysical Exploration, Geophysical Prospecting
    Language: English
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  • 87
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell
    Associated volumes
    Call number: 9/M 93.0659 ; 9/M 92.0431
    In: Geological Society special publication
    Description / Table of Contents: In recognition of the increasing interest in the subject of deformation of sediments and sedimentary rocks shown by Earth scientists in recent years, a major international conference with this theme was held at University College London in April 1985. This volume contains the texts of those contributions to the Conference that were submitted for publication. The collection of papers presented is not a complete record of the proceedings, as some contributors chose not to submit a manuscript. However, most important subject areas are represented, and the papers provide both a review of the present state of the art and pointers for future investigation. The articles have been grouped into three main divisions: experimental and theoretical, process orientated, and descriptive of particular areas or localities. Within those groupings there is no particular significance in the order of printing except that articles with aspects in common have been placed near to one another. Studies of naturally deformed sedimentary rocks repeatedly indicate that much of the observed deformation resulted from processes active before the rock was lithified. An understanding of the origins of these structures cannot be established using the principles of rock mechanics and crystal physics commonly employed in ‘hard-rock’ structural geology (Rutter 1976; White 1976), the principles of the engineering discipline of soil mechanics being more appropriate. Alternatively, the post-lithification deformation of sediments is a typical rock mechanics problem and may involve an understanding of elasticity (Jaeger & Cook 1969), fracturing (Price 1966; Barton 1976), crystal plasticity (Turcotte & Schubert 1982) and diffusion based deformation mechanisms (Rutter 1976, 1983). The student of sediment deformation must therefore be conversant with all aspects of rock and soil deformation. The Conference, with its contributions by structural geologists, sedimentologists, geotechnical engineers and those conversant with specific aspects of rock and soil mechanics, provided a coverage of this very wide subject area. This is reflected in the contents of the volume.
    Type of Medium: Monograph available for loan
    Pages: VII, 350 S. , Ill., graph. Darst., Kt.
    ISBN: 0632017333
    Series Statement: Geological Society special publication 29
    Classification:
    Tectonics
    Language: English
    Note: Mervyn E. Jones and R. M. F. Preston: Introduction / Geological Society, London, Special Publications, 29:1-8, doi:10.1144/GSL.SP.1987.029.01.01 --- Part I: Theory and Experimental --- G. Owen: Deformation processes in unconsolidated sands / Geological Society, London, Special Publications, 29:11-24, doi:10.1144/GSL.SP.1987.029.01.02 --- J. P. Gratier: Pressure solution-deposition creep and associated tectonic differentiation in sedimentary rocks / Geological Society, London, Special Publications, 29:25-38, doi:10.1144/GSL.SP.1987.029.01.03 --- G. Mandl and R. M. Harkness: Hydrocarbon migration by hydraulic fracturing / Geological Society, London, Special Publications, 29:39-53, doi:10.1144/GSL.SP.1987.029.01.04 --- C. R. I. Clayton and M. C. Matthews: Deformation, diagenesis and the mechanical behaviour of chalk / Geological Society, London, Special Publications, 29:55-62, doi:10.1144/GSL.SP.1987.029.01.05 --- R. J. Allison: Non-destructive determination of Young’s modulus and its relationship with compressive strength, porosity and density / Geological Society, London, Special Publications, 29:63-69, doi:10.1144/GSL.SP.1987.029.01.06 --- Alex J. Maltman: A laboratory technique for investigating the deformation microstructures of water-rich sediments / Geological Society, London, Special Publications, 29:71-76, doi:10.1144/GSL.SP.1987.029.01.07 --- Alex. J. Maltman: Shear zones in argillaceous sediments—an experimental study / Geological Society, London, Special Publications, 29:77-87, doi:10.1144/GSL.SP.1987.029.01.08 --- Part II: Processes --- John R. Underhill and Nigel H. Woodcock: Faulting mechanisms in high-porosity sandstones; New Red Sandstone, Arran, Scotland / Geological Society, London, Special Publications, 29:91-105, doi:10.1144/GSL.SP.1987.029.01.09 --- Jean-Pierre Petit and Edgard Laville: Morphology and microstructures of hydroplastic slickensides in sandstone / Geological Society, London, Special Publications, 29:107-121, doi:10.1144/GSL.SP.1987.029.01.10 --- Michel Guiraud and Michel Séguret: Soft-sediment microfaulting related to compaction within the fluviodeltaic infill of the Soria strike-slip basin (northern Spain) / Geological Society, London, Special Publications, 29:123-136, doi:10.1144/GSL.SP.1987.029.01.11 --- Michael Leeder: Sediment deformation structures and the palaeotectonic analysis of sedimentary basins, with a case-study from the Carboniferous of northern England / Geological Society, London, Special Publications, 29:137-144, NP, 145-146, doi:10.1144/GSL.SP.1987.029.01.12 --- Pierre Labaume: Syn-diagenetic deformation of a turbiditic succession related to submarine gravity nappe emplacement, Autapie Nappe, French Alps / Geological Society, London, Special Publications, 29:147-163, doi:10.1144/GSL.SP.1987.029.01.13 --- S.A. Schack Pedersen: Comparative studies of gravity tectonics in Quaternary sediments and sedimentary rocks related to fold belts / Geological Society, London, Special Publications, 29:165-179, doi:10.1144/GSL.SP.1987.029.01.14 --- S. G. Farrell and S. Eaton: Slump strain in the Tertiary of Cyprus and the Spanish Pyrenees. Definition of palaeoslopes and models of soft-sediment deformation / Geological Society, London, Special Publications, 29:181-196, doi:10.1144/GSL.SP.1987.029.01.15 --- P. M. Clifford, M. C. Rice, L. L. Pryer, and F. Fueten: Mass transfer in unmetamorphosed carbonates and during low-grade metamorphism of arenites / Geological Society, London, Special Publications, 29:197-209, doi:10.1144/GSL.SP.1987.029.01.16 --- Part III: Descriptive --- K. T. Pickering: Wet-sediment deformation in the Upper Ordovician Point Leamington Formation: an active thrust-imbricate system during sedimentation, Notre Dame Bay, north-central Newfoundland / Geological Society, London, Special Publications, 29:213-218,NP,219-232,NP,234-239, doi:10.1144/GSL.SP.1987.029.01.17 --- Krzysztof Brodzikowski, Roman Gotowała, Ludwik Kasza, and Antonius J. Van Loon: The Kleszczów Graben (central Poland): reconstruction of the deformational history and inventory of the resulting soft-sediment deformational structures / Geological Society, London, Special Publications, 29:241-254, doi:10.1144/GSL.SP.1987.029.01.18 --- K. Brodzikowski, R. Gotowała, A. Hałuszczak, D. Krzyszkowski, and A. J. Van Loon: Soft-sediment deformations from glaciodeltaic, glaciolacustrine and fluviolacustrine sediments in the Kleszczów Graben (central Poland) / Geological Society, London, Special Publications, 29:255-267, doi:10.1144/GSL.SP.1987.029.01.19 --- Krzysztof Brodzikowski, Dariusz Krzyszkowski, and Antonius J. Van Loon: Endogenic processes as a cause of penecontemporaneous soft-sediment deformations in the fluviolacustrine Czyżów Series (Kleszczów Graben, central Poland) / Geological Society, London, Special Publications, 29:269-278, doi:10.1144/GSL.SP.1987.029.01.20 --- Krzysztof Brodzikowski and Andrzej Hałuszczak: Flame structures and associated deformations in Quaternary glaciolacustrine and glaciodeltaic deposits: examples from central Poland / Geological Society, London, Special Publications, 29:279-286, doi:10.1144/GSL.SP.1987.029.01.21 --- Krzysztof Brodzikowski, Andrzej Hałuszczak, Dariusz Krzyszkowski, and Antonius J. Van Loon: Genesis and diagnostic value of large-scale gravity-induced penecontemporaneous deformation horizons in Quaternary sediments of the Kleszczów Graben (central Poland) / Geological Society, London, Special Publications, 29:287-298, doi:10.1144/GSL.SP.1987.029.01.22 --- Colin A. Davenport and Philip S. Ringrose: Deformation of Scottish Quaternary sediment sequences by strong earthquake motions / Geological Society, London, Special Publications, 29:299-314, doi:10.1144/GSL.SP.1987.029.01.23 --- J. Alexander: Syn-sedimentary and burial related deformation in the Middle Jurassic non-marine formations of the Yorkshire Basin / Geological Society, London, Special Publications, 29:315-324, doi:10.1144/GSL.SP.1987.029.01.24 --- Bill Fitches: Aspects of veining in the Welsh Lower Palaeozoic Basin / Geological Society, London, Special Publications, 29:325-342, doi:10.1144/GSL.SP.1987.029.01.25
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  • 88
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: 4/M 92.1327/16 ; ILP/M 06.0119
    In: Geodynamics series
    In: Publication of the International Lithosphere Programme
    Type of Medium: Monograph available for loan
    Pages: xi, 327 S. : graph. Darst.
    ISBN: 0875905188
    Series Statement: Geodynamics series 16
    Classification:
    Geophysical Deep Sounding
    Language: English
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  • 89
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : Wiley
    Call number: 19/O 6665
    Type of Medium: Monograph available for loan
    Pages: XXIII, 440 S. : graph. Darst.
    ISBN: 0471861871
    Series Statement: Wiley series in probability and mathematical statistics : Probability and mathematical statistics
    Language: English
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  • 90
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 12/MOP 38868 ; MOP 38868/7 ; MOP 38868/7(2. Ex.)
    In: World survey of climatology, Vol. 7
    Type of Medium: Monograph available for loan
    Pages: XI, 443 S.
    ISBN: 0444415165
    Series Statement: World survey of climatology 7
    Language: English
    Note: Contents: Acknowledgements. - 1. Introduction. - Soviet climatological thought. - Content and organization of this volume. - References and further reading. - 2. General analysis of climatic controls. - Atmospheric circulation over the U.S.S.R. - Fronts, cyclones, and anticyclones. - Winter. - Summer. - Air masses and regionalization. - References and further reading. - 3. European U.S.S.R. and Western Siberia. - Definition of the region. - Circulation features. - Cyclogenesis and cyclone tracks. - Synoptic situations and associated air masses. - Air flows. - Air masses. - Moisture flux. - Subregions. - The south. - Nature of the region, Air masses, Cloudiness and precipitation, Wind, Weather types. - The central region. - Carpathians, Weather types. - The European northwest. - The European northeast. - The Urals. - Western Siberia. - The tundra zone, The forest zone, The steppe zone. - References and further reading. - 4. Eastern Siberia. - Definition of the region. - Pressure systems and weather. - Winter. - Spring. - Summer. - Autumn. - Regional description. - References and further reading. - 5. Far East. - Introduction. - Atmospheric circulation and precipitation processes. - Climatic regions. - The southwestern region. - The northeastern region. - References and further reading. - 6. Central Asia. - Definition of the region. - General atmospheric flow and synoptic processes. - Cyclonic storms. - Local winds. - Moisture conditions. - Precipitation regime. - Snow and ice. - Thunderstorms and hail. - Clouds and fog. - Thermal conditions. - References and further reading. - 7. The Caucasus. - Topography. - Atmospheric circulation. - Local circulations and associated weather. - Precipitation. - Sunshine, clouds, and precipitation frequencies. - Fog, snow, glaze, and thunderstorms. - Radiation and temperature. - Climatic regions of the Caucasus. - Northern Caucasus. - The high mountain zone of the Great Caucasus. - Western Transcaucasus. - Eastern Transcaucasus. - The Talysh region. - The Armenian Plateau and the Lesser Caucasus. - References and further reading. - 8. The thermal factor. - Radiation components. - Global radiation. - Direct and scattered radiation. - Reflectivity, absorption, and terrestrial radiation. - Heat balance at the earth's surface. - Radiation balance. - Heat expended on evaporation. - Turbulent heat exchange. - Heat advection. - Latent heat. - Sensible heat. - Temperature. - Temperature means. - Temperature anomalies. - Temperature variations. - Critical temperatures. - References and further reading. - 9. The moisture factor. - Atmospheric moisture content and moisture flux. - Moisture content and moisture flux over European U.S.S.R. - Humidity. - Clouds and fog. - Fog. - Precipitation. - Frequency, intensity, and duration. - Variability. - Precipitation type. - Thunderstorms and hail, Snow, Glaze and rime. - Water losses. - Evaporation. - Stream runoff. - Moisture balance, drought, and sukhovey. - References and further reading. - 10. Wind. - References and further reading. - 11. Climate distribution. - Classification schemes. - The Grigor'yev-Budyko scheme. - Moisture distribution. - Thermal distribution. - Climatic regions. - References and further reading. - Appendix - climatic tables. - Reference Index. - Geographical index. - Subject index.
    Location: Reading room
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  • 91
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 12/MOP 38868/6
    In: World survey of climatology
    Type of Medium: Monograph available for loan
    Pages: IX, 248 S.
    ISBN: 0444413367
    Series Statement: World survey of climatology 6
    Language: English
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  • 92
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: 5/G 8861/2
    In: Geomagnetism
    Type of Medium: Monograph available for loan
    Pages: xviii, 579 S.
    ISBN: 012378672X
    Classification:
    Geomagnetism, Geoelectromagnetism
    Language: English
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  • 93
    Monograph available for loan
    Monograph available for loan
    Washington, DC : American Geophysical Union
    Associated volumes
    Call number: 4/M 92.1327/10
    In: Geodynamics series
    Type of Medium: Monograph available for loan
    Pages: 310 S. + 3 Kt.-Beil.
    ISBN: 0875905102
    Series Statement: Geodynamics series 10
    Classification:
    Geodynamics
    Language: English
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  • 94
    Monograph available for loan
    Monograph available for loan
    Oxford [u.a.] : Blackwell Scientific Publications
    Associated volumes
    Call number: 9/M 93.0660
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: X, 230 S. , zahlr. Ill. u. graph. Darst. u. Kt.
    ISBN: 0632018062
    Series Statement: Geological Society special publication 34
    Classification:
    Applied Geology
    Language: English
    Note: J. C. Goff and B. P. J. Williams: Introduction / Geological Society, London, Special Publications, 34:NP, doi:10.1144/GSL.SP.1987.034.01.01 --- Section 1: Fluid Flow in Compacting Basins --- Richard E. Chapman: Fluid flow in sedimentary basins: a geologist’s perspective / Geological Society, London, Special Publications, 34:3-18, doi:10.1144/GSL.SP.1987.034.01.02 --- Kinji Magara: Fluid flow due to sediment loading—an application to the Arabian Gulf region / Geological Society, London, Special Publications, 34:19-28, doi:10.1144/GSL.SP.1987.034.01.03 --- Section 2: Fluid Flow in the Western Canadian Sedimentary Basin --- Brian Hitchon, S. Bachu, C. M. Sauveplane, and A. T. Lytviak: Dynamic basin analysis: an integrated approach with large data bases / Geological Society, London, Special Publications, 34:31-44, doi:10.1144/GSL.SP.1987.034.01.04 --- J. Tóth and T. Corbet: Post-Palaeocene evolution of regional groundwater flow systems and their relation to petroleum accumulations, Taber Area, southern Alberta, Canada / Geological Society, London, Special Publications, 34:45-77, doi:10.1144/GSL.SP.1987.034.01.05 --- F. W. Jones and J. A. Majorowicz: Some aspects of the thermal regime and hydrodynamics of the western Canadian sedimentary basin / Geological Society, London, Special Publications, 34:79-85, doi:10.1144/GSL.SP.1987.034.01.06 --- Harry J. Bradbury and Grant R. Woodwell: Ancient fluid flow within foreland terrains / Geological Society, London, Special Publications, 34:87-102, doi:10.1144/GSL.SP.1987.034.01.07 --- Section 3: Fluid Flow in United Kingdom Groundwater Basins --- R. A. Downing, W. M. Edmunds, and I. N. Gale: Regional groundwater flow in sedimentary basins in the U.K. / Geological Society, London, Special Publications, 34:105-125, doi:10.1144/GSL.SP.1987.034.01.08 --- A. H. Bath, A. E. Milodowski, and G. E. Strong: Fluid flow and diagenesis in the East Midlands Triassic sandstone aquifer / Geological Society, London, Special Publications, 34:127-140, doi:10.1144/GSL.SP.1987.034.01.09 --- Michael Price: Fluid flow in the Chalk of England / Geological Society, London, Special Publications, 34:141-156, doi:10.1144/GSL.SP.1987.034.01.10 --- N. P. Wilson and M. N. Luheshi: Thermal aspects of the East Midlands aquifer system / Geological Society, London, Special Publications, 34:157-169, doi:10.1144/GSL.SP.1987.034.01.11 --- Section 4: Fluid Flow in Low Permeability and Fractured Media --- J. Alexander, J. H. Black, and M. A. Brightman: The role of low-permeability rocks in regional flow / Geological Society, London, Special Publications, 34:173-183, doi:10.1144/GSL.SP.1987.034.01.12 --- J. H. Black: Flow and flow mechanisms in crystalline rock / Geological Society, London, Special Publications, 34:185-200, doi:10.1144/GSL.SP.1987.034.01.13 --- David A. Brown: The flow of water and displacement of hydrocarbons in fractured chalk reservoirs / Geological Society, London, Special Publications, 34:201-218, doi:10.1144/GSL.SP.1987.034.01.14
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  • 95
    Call number: 5/M 92.1329(41)
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: X, 250 S. : Ill., graph. Darst.
    ISBN: 0875900674
    Series Statement: Geophysical monograph 41
    Classification:
    Tectonics
    Language: English
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  • 96
    Monograph available for loan
    Monograph available for loan
    Karlsruhe
    Associated volumes
    Call number: M 91.1642 7 Fach 10
    In: International Lithosphere Program
    Type of Medium: Monograph available for loan
    Pages: 62 S.
    Language: English
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  • 97
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: M 91.1643 / Regal 10
    In: International Lithosphere Program
    Type of Medium: Monograph available for loan
    Pages: 182 S.
    Language: English
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  • 98
    Monograph available for loan
    Monograph available for loan
    Washington : American Geophysical Union [u.a.]
    Associated volumes
    Call number: 5/M 92.1329/39
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: VII, 486 S.
    ISBN: 0875900666
    Series Statement: Geophysical monograph 39
    Language: English
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  • 99
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/18
    In: CRREL Report, 83-18
    Description / Table of Contents: An evaluation of an impulse radar system for detecting cavities under concrete pavement is discussed, and field results are presented. It was found that a dual antenna mode of surveying was ideal for void detection. In this mode one antenna operated in a transceive mode and a second, offset from the first, operated in a receive-only mode. This arrangement allowed a refraction-type profile survey to be performed, which enabled subpavement voids to be easily detected. Field trails were held at Plattsburgh Air Force Base, where 28 cavities were detected and mapped. Drilling of holes verified that a cavity existed and allowed cavity depth to be measured. The cavities varied from 1.5 in. to 23 in, depth and were up to 20 ft. long.
    Type of Medium: Series available for loan
    Pages: 49 Seiten , Illustrationen
    Series Statement: CRREL Report 83-18
    Language: English
    Note: CONTENTS Abstract Preface Introduction Plattsburgh Air Force Base Radar sounding system Survey procedure Cavity inspection Radar cavity detection test Radar profile results Falling-weight deflectometer tests Discussion and conclusions Literature cited
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  • 100
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-83/12
    In: CRREL Report, 83-12
    Description / Table of Contents: This paper documents the development and verification of two finite difference models that solve the general two-dimensional form of the heat conduction equation, using the alternative-direction implicit method. Both can handle convective, constant flux, specified temperature and semi-infinite boundaries. The conducting medium may be composed of many materials. The first program, ADI, solves for the case where no change of state occurs. ADIPC solves for case where a freeze/thaw change of phase may occur, using the apparent heat capacity method. Both models are verified by comparison to analytical results.
    Type of Medium: Series available for loan
    Pages: 74 Seiten , Illustrationen
    Series Statement: CRREL Report 83-12
    Language: English
    Note: CONTENTS Abstract Preface Introduction Finite differences applied to heat transfer Heat conduction equation Boundary conditions Phase change Computer program ADDATA, the data subroutine TRIDIG, the matrix solver ISOTHM, the isotherm finider ADI, main program ADEPC, main program Verification of ADI Comparison of ADI with analytical results Comparison of ADI with experimental results Verification of ADIPC Comparison of ADIPC with analytical results-the Neumann solution Comparison of ADIPC with analytical results-two-dimensional phase change verification User instruction for ADI User instruction for ADIPC Conclusions Literature cited Appendix A. Program INFSUM and sample input and output for program ADI Appendix B. Program ADIPC and sample input and output
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