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  • Books  (4,967)
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  • 1965-1969  (1,403)
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  • Books  (4,967)
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  • 1
    Monograph available for loan
    Monograph available for loan
    Carbonate rocks (1967)
    Amsterdam [u.a.] : Elsevier
    Associated volumes
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    Call number: 9/M 13.0083
    In: Developments in sedimentology
    Type of Medium: Monograph available for loan
    Pages: 471 S., Ill., graph. Darst., kt-.
    Series Statement: Developments in sedimentology 9A
    Language: English
    Location: Reading room
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  • 2
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    Publications on geodesy (1)
    Delft ; 1.1969-76.2010
    Details Availability
    Call number: S 90.0083
    ISSN: 0165-1706
    URL: http://www.ncg.knaw.nl/eng/publications/geodesy.html
    Language: English
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  • 3
    Monograph available for loan
    Monograph available for loan
    Proceedings of SESAME opening meeting at Boulder, Colorado : Sept. 4-6, 1974 (1975)
    Boulder, Colo. : Environmental Research Laboratories
    Details Availability
    Call number: MOP 41125 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VIII, 499 Seiten
    Language: English
    Location: MOP - must be ordered
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  • 4
    Series available for loan
    Series available for loan
    Interpretation of young ice forms in the Gulf of St. Lawrence using side-looking airborne radar and infrared imagery (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-337
    In: Research report
    Description / Table of Contents: Contents: Introduction. - Surface ice observations. - Imagery interpretation. - Side-looking airborne radar. - Infrared. - Conclusions. - Literature cited.
    Description / Table of Contents: Ice conditions during mid-January 1974 in the Gulf of St. Lawrence and in the estuaty as far upstream as Rimouski are described utilitizing side-looking airborne radar, infrared and photographic imagery. The interpretations were verified by simultaneous surface observations on the ice by investigators operating from the CSS Dawson. The ice examined was undergoing rapid drift and deformation and showed a wide variety of thin ice (0-40 cm) features formed under the influence of strong winds and currents. These observations should serve as a guide in interpreting ice conditions in similar areas where ground truth data are not available.
    Type of Medium: Series available for loan
    Pages: 41 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 337
    URL: http://www.worldcat.org/oclc/2327064
    Language: English
    Branch Library: AWI Library
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  • 5
    Series available for loan
    Series available for loan
    Compressibility characteristics of undisturbed snow (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-336
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Nomenclature. - Introduction. - Description of study. - Sample preparation. - Test equipment and procedure. - Discussion of results. - Stress-density relationship. - Effect of rate of deformation. - Effect of temperature. - Effect of initial snow density. - Stress-deformation relationship. - Summary and conclusions. - Microstructural analysis. - Introduction. - Analytical methods. - Results and discussion. - Conclusion. - Literature cited. - Anpendix: Test data.
    Description / Table of Contents: The effects of snow temperature, rate of deformation, and initial density on the stress vs density and stress vs deformation relationships were investigated in the pressure range of 0.1 to 75 bars. The rate of deformation in the range of 0.027 to 27 cm sec^-1 does not have a significant effect. A decrease in temperature in the range of 0° to -40°C increases the resistance to stress and deformation, the temperature effect increasing with applied pressure and initial density. The effect of initial density is significant. For any stress, an increase in the initial density results in an increase in the resulting density, particularly at low stress levels and at temperatures near 0°C. The texture of artificially compacted snow is significantly different from that of naturally compacted snow of the same density because of the very short recrystallization time period.
    Type of Medium: Series available for loan
    Pages: iv, 57 Seiten , Illustrations
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 336
    URL: http://www.worldcat.org/oclc/1035634745
    Language: English
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  • 6
    Series available for loan
    Series available for loan
    Microspherules in snow and ice-fog crystals (1969)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-245
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Snow crystals in Greenland. - Microspherules. - Microspherules in snow and ice-fog crystals. - Concentration and radii of spherules. - Discussion and conclusions. - Literature cited.
    Description / Table of Contents: Spherules found in snow crystals, ice-fog crystals, fallout particles, and fly ash were studied with an electron microscope using the electron diffraction method. The central part of the residues of 1004 specimens of natural snow crystals from Greenland, the United States, and Japan were examined; 14 spherules 0.1 to 1.5? in radius were found among them. The residues of 658 artificial ice-fog crystals formed from water vapor in flue gases of coal-burning electric power plants at Fairbanks, Alaska, were also examined; nine spherules were found. Spherules similar to those found in ice-fog residues were found in furnace-produced fly ash fallout at Fairbanks, Alaska. Electron and optical microscope examination of spherules found in Greenland snow reveals a size distribution of the form dN/d(log r) = Cr-ß where ß approximately 3. The properties of spherules and the mean mass of snow crystals from Greenland are described. The electron microscope study indicated that less than 0.7% of the 1004 snow crystals contained spherules of possible extraterrestrial origin, and that snow crystals are formed mainly on clay mineral particles by heterogeneous nucleation.
    Type of Medium: Series available for loan
    Pages: iv, 10 Seite , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 245
    URL: https://apps.dtic.mil/sti/citations/tr/AD0691326
    Language: English
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  • 7
    Series available for loan
    Series available for loan
    Bubble coalescence in ice as a tool for the study of its deformation history (1968)
    Hanover, NH : U.S. Army Materiel Command Cold Regions Research & Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-251
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Theory. - Application to ice sheets and ice shelves. - Summary. - Literature cited.
    Description / Table of Contents: An analysis is made of the rate of bubble coalescence in a deforming ice mass. A total strain of at least 8 is required before appreciable coalescence occurs, The analysis has.been applied to deforming ice shelves and ice sheets. No appreciable coalescence is expected in ice shelves but coalescence should occur in ice sheets (or glaciers) if the shear strain rate at the bottom surface is of the order of 0.075/yr or larger. Measurements of bubble concentration are capable of setting limits on paleo-strain rates of the present ice sheets. Bubble migration down temperature gradients presents complications to the study of bubble coalescence.
    Type of Medium: Series available for loan
    Pages: iv, 5 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 251
    URL: https://dx.doi.org/10.3189/S0022143000030951
    Language: English
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  • 8
    Series available for loan
    Series available for loan
    Aerial sensing and photographic study of the El Verde rain forest, Puerto Rico (1969)
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-250
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Methods. - Results. - Ground and aerial photography. - Hemispherical photography. - Light quality. - Discussion. - Literature cited. - Abstract.
    Description / Table of Contents: Aerial and ground photographs were taken over a 2-year period of sites in the El Verde rain forest to record the consistency of the vegetational patterns in untreated sites and the changes that occurred following gamma irradiation. Four emulsions were used: panchromatic infrared, false color transparency and color transparency. Densitometry was used to evaluate color film and the vegetation response to 3 months of radiation. The color emulsions provided the sharpest indication of damage to vegetation and the succession following treatment. Hemispherical photography of the canopy was evaluated in terms of a canopy cover index defined as percent of light passing through the negative in a 90-degree cone area. Control stations were remarkably constant in all photography, establishing the stability and slow natural changes in rain forest structure. Spectral light measurements within the forest confirmed the predominance of far red shade light. Compared to similar studies on the chronic irradiated forest at Brookhaven National Laboratory the El Verde results were less distinct.
    Type of Medium: Series available for loan
    Pages: iii, 21 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 250
    URL: https://www.worldcat.org/de/title/3298743
    Language: English
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  • 9
    Series available for loan
    Series available for loan
    Electrolytic conductivity of snow and glacier ice from Antarctica and Greenland (1968)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-248
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Literature cited.
    Description / Table of Contents: Conductivity measurements have been made on snow and ice samples from pits and deep drillholes at a number of localities in Antarctica and Greenland. Conductivities of the order 1-2 [My]mho/cm only were recorded at the inland sites. Data from deep cores representing more than 1900 years of continuous snow accumulation at Byrd Station, Antarctica, and more than 400 years deposition at Inge Lehmann, Greenland, showed no significant variations of conductivity with time. Measurements of freshly precipitated snow from a single coastal location in McMurdo Sound, Antarctica, also yielded relatively low conductivities of the order 3-4 [My]mho/cm. The substantial increase observed in the conductivity of core samples from near the surface of the Ross Ice Shelf at Little America V can be attributed most probably to windborne salts of marine origin that had accumulated on the surface after the snow was deposited. A peak conductivity of 49 [My]mho/cm was recorded in snow estimated to have been deposited within 20 km of the seaward edge of the Ross Ice Shelf and the maritime effect could still be detected in samples deposited more than 40 km from the ice front. For samples deposited at distances of greater than 200 km from the edge of the Ross Ice Shelf conductivities never exceeded 2 [My]mho/cm. The very low conductivities observed in ice cores from near the bottom of the Ross Ice Shelf confirm earlier conclusions based on detailed petrographic studies oi the cores that the 258-m-thick ice shelf at Little America V is composed entirely of glacial ice.
    Type of Medium: Series available for loan
    Pages: iv, 8 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 248
    URL: https://dx.doi.org/10.1029/JB073i012p03643
    Language: English
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  • 10
    Series available for loan
    Series available for loan
    Hydrology of a drainage basin on the Alaskan coastal plain (1968)
    Hanover, NH : US Army Materiel Command, Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-240
    In: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command, 240
    Description / Table of Contents: A 4-summer hydrologic record from a 1.6 km^2 drainage basin at Barrow, Alaska is analyzed. The watershed, a drained lake basin, is underlain by continuous permafrost within 0.3m of the tundra surface and is covered by ice-wedge polygons and numerous small shallow ponds. Considerable variations from the 20-yr means of summer climate (thaw period 88 days, precipitation 67 mm) are represented in the data: 1963 - cold, extremely wet; 1964 - cold, extremely dry; 1965 - cool, dry; 1966 - cool, wet. Runoff varied greatly from storm to storm, occurring primarily through and over the tundra mat and through an intricate system of polygonal troughs and ponds. As a result of the subdued coastal topography, varying areas (0.3 km^2 to 1.6 km^2) contribute to runoff from different storms. Analyses of hydrographs revealed: 1) lag times generally from 3 to 10 hr; 2) recession constants of about 50 hr, but occasionally as much as 160 hr; and 3) runoff from individual storms between 1 and 70%. About 5% of the thaw season precipitation normally runs off. Comparison of total thaw season precipitation between the U.S. Weather Bureau and a shielded gage located on the watershed indicated no major differences. If "trace" precipitation is considered, only 90% of the actual precipitation may be recorded. Pan evaporation for an average thaw season is about 160 mm and evapotranspiration which is essentially in balance with precipitation is about 60 mm. Conductivity of runoff water varied from 250 [My]mhos during sustained discharge to more than 500 [My]mhos during low flows in dry years. Precipitation chemistry showed no correlation with storm direction. Assuming all winter precipitation runs off, and the data are spatially and temporally representative, about 50% of the measured annual precipitation in this region runs off into the Arctic Ocean.
    Type of Medium: Series available for loan
    Pages: IV, 18 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 240
    URL: https://hdl.handle.net/11681/5946
    Language: English
    Note: CONTENTS: Preface. - Summary. - Introduction. - Regional setting. - Description of watershed. - Climatic record. - Methods. - Precipitation. - Water and air temperatures. - Discharge. - Evaporation and pond levels. - Water chemistry. - Soil thaw. - Results and discussion. - Precipitation. - Runoff. - Evaporation and transpiration. - Water chemistry. - Conclusions. - Literature cited.
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  • 11
    Series available for loan
    Series available for loan
    Variation of some mechanical properties of polar snow, Camp Century, Greenland (1969)
    Hanover, NH : U.S. Army Corps of Engineers, Cold Regions Research and Engineering Laboratory
    Associated volumes
    Details Availability
    Call number: ZSP-202-276
    In: Research report
    Description / Table of Contents: CONTENTS: Introduction. - Test site. - Test procedures. - Equipment. - Unconfined compression tests. - Ring tensile tests. - Test results. - Unconfined compression tests. - Ring tensile tests. - Discussion. - Literature cited. - Appendix A. Calculation of the effect of nonaxial loading of unconfined compression specimens. - Appendix B. Camp Century unconfined compressive strength data at -25C. - Appendix C. Camp Century ring-tensile strength data at -25C. - Appendix D. Unconfined compressive strength of Camp Century vertical snow samples 8.25 in. length, 3.0 in. diam at -25C. - Abstract.
    Description / Table of Contents: The unconfined compressive strengths [Sigma]c and the ring-tensile strengths [Sigma]T of snow and ice specimens from the Inclined Drift at Camp Century, Greenland, were determined. The specimen densities varied over essentially the complete natural density range of polar snow and ice (0.340 to 0.890 g/cm^3). The specimens were loaded rapidly to failure with times varying between 0.2 and 1.4 sec. During loading, head speeds varied between 5.1 and 23.6 cm/min, although during individual tests they were constant. Even the low density specimens failed in the brittle mode. Although a plot of [Sigma]T vs [Gamma] is linear, [Sigma]c vs [Gamma] is clearly nonlinear. This nonlinearity may result from either changes in the level of the internal stress concentrations associated with the voids in the snow or from changes in the ratio (bulk porosity/effective porosity of the failure surface) with density. Both tangent and secant moduli are linear functions of [Gamma]. There is no pronounced change in [Sigma]c with changes in strain rate. A significant increase in [Sigma]T, [Sigma]c and the modulus values was noted at bulk densities greater than 0.830 g/cm^3. This increase is presumably caused by the close-off of the air passages.
    Type of Medium: Series available for loan
    Pages: 35 Seiten , Illustrationen, graphische Darstellungen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 276
    URL: http://www.worldcat.org/oclc/5974547
    Language: English
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  • 12
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    Series available for loan
    Bubbles and bubble pressures in Antarctic glacier ice (1968)
    Hanover, NH : U.S. Army Materiel Command, Terrestrial Sciences Center, Cold Regions Research & Engineering Laboratory
    Associated volumes
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    Call number: ZSP-202-249
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Abstract. - Introduction. - Analytical procedures. - Results and discussion. - Bubbles in ice. - Conclusions. - Literature cited.
    Description / Table of Contents: Application of the gas law to fourth-place density measurements of ice samples from two deep drill holes at Byrd Station and Little America V, Antarctica, shows that virtually all density increase beyond the pore close-off density (0.830 g/cm^3) can be attributed to compression of the entrapped bubbles of air. Data from Byrd Station also indicate that the lag between overburden pressure and bubble pressure, initially 4-5 kg/cm^2 at pore close-off, diminishes to less than 1.0 kg/cm^2 at about 200-m depth. By substituting the overburden pressure for the bubble pressure in the pressure-density relationship based on the gas law, ice densities below 200 m can be calculated more accurately than they can be measured per se on cores because of the relaxation that occurs in samples recovered from high confining pressures. This relaxation, resulting in a progressive increase in the bulk volume of the ice with time, is generally attributed to decompression of the entrapped air bubbles following removal of the ice from high confining pressures. However, calculations of the stress in ice due to bubble pressure, together with measurements of bubble sizes in cores from various depths at Byrd Station, both tend to indicate that there has'been negligible decompression of the inclosed bubbles. It is suggested that most of this relaxation may be due to the formation of microcracks in the ice. Anomalous bubble pressure-density relations at Little America V tend to confirm abundant stratigraphic evidence of the existence of considerable deformation in the upper part of the Ross Ice Shelf. Studies of crystal-bubble relations at Byrd Station revealed that the concentration of bubbles in ice remains remarkably constant at approximately 220 bubbles per cm^3. Bubbles and crystals were found to be present in approximately equal numbers at pore close-off at 64-m depth, at which level the average bubble diameter was 0.95 mm, decreasing to 0.49 mm at 116 m and to 0.33 mm at 279 m. Despite a tenfold increase in the size of crystals between 64 and 279 m, the bubbles showed no tendency to migrate to grain boundaries during recrystallization of the ice. The observation that most of the bubbles had assumed substantially spherical shapes by 120-m depth points to essentially hydrostatic conditions in the upper layers of the ice sheet at Byrd Station.
    Type of Medium: Series available for loan
    Pages: iv, 16 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 249
    URL: https://www.worldcat.org/de/title/6023806
    Language: English
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  • 13
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    The bearing capacity of floating ice plates subjected to static or quasi-static loads : a critical survey (1975)
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-333
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Introduction. - Analogy method. - Method based on the bending theory of elastic plates and the criterion [Sigma]max = [Sigma]f. - Methods based on viscoelastic theories. - Methods based on the yield line theory or limit analysis. - Comparison of analytical and test results. - General remarks. - Effect of bending and shearing forces on deflection of an ice cover. - Determination of Pf(O). - Determination of Pf(t). - Determination of [Sigma]f. - Summary and recommendations. - Literature cited.
    Description / Table of Contents: This report contains a critical survey of the literature on the bearing capacity of floating ice plates. It consists of a discussion of general questions, a critical survey of analytical attempts to determine the bearing capacity of floating ice plates, and a survey of field and laboratory tests on floating ice plates and their relation to the analytical results. The paper concludes with a systematic summary of the results, a discussion of observed shortcomings, and suggestions for needed investigations.
    Type of Medium: Series available for loan
    Pages: iv, 43 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 333
    URL: http://www.worldcat.org/oclc/1387849
    Language: English
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  • 14
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    Fracture of lake and sea ice (1969)
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research & Engineering Laboratory
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    Call number: ZSP-202-269
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - List of symbols. - Introduction. - Structure of ice and ice sheets. - Ice as a mineral. - Lake and sea ice. - Chemistry and phase relations. - Dislocations,cracks,and stress concentrators. - Direct observation of dislocations. - Crackformation. - Stress concentration. - Theoretical considerations. - Experimental results. - Compressive strength. - Indentation failure. - Tensile strength. - Flexural strength. - Shear strength. - Impact strength. - Scale effects. - Strength deterioration in the spring. - Recommended research. - Summary. - Selected bibliography. - Abstract.
    Description / Table of Contents: The increased activity in cold regions has made a thorough understanding of fracture in lake and sea ice quite desirable, inasmuch as this information has application to a number of problems of geophysical as well as engineering importance. This survey starts with a discussion of the structure of ice I and the macro- and microstructure of sea and lake ice as well as their chemistry and phase relations. Recent work on the direct observation of dislocations as well as the formation of cracks in ice is summarized. Formal ice-brine-air models for analyzing variations in ice strength are also reviewed. The results of the different types of tests are discussed and cornpared (compressive, indentation, direct and ring-tension, small beam flexure and in situ cantilevers and simple beams, shear, and impact). Scale effects are considered as well as the rapid strength deterioration experienced by ice sheets in the spring. Finally, a number of recommendations are made concerning future research in this field.
    Type of Medium: Series available for loan
    Pages: viii, 79 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 269
    URL: http://www.worldcat.org/oclc/647427544
    Language: English
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  • 15
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    Geology of the Hot Springs quadrangle Fall River and Custer Counties, South Dakota (1967)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1063-K)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S. 427-442 + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1063-K
    Language: English
    Location: Lower compact magazine
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  • 16
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    Structural map of the southwestern sector of the Marguarés Massif - Ligurian Alps - 1:10 000 (1983)
    Details Availability
    Call number: K 97.0350
    Series Statement: Memorie della Societa Geologica Italiana 25, 1983, tav. 1
    Language: Italian
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  • 17
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    Geology of the Potosi quadrangle, Grant County Wisconsin, and Dubuque County, Iowa (1966)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1123-I)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV S., S.533-571 + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 1123-I
    Language: English
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  • 18
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    Quicksilver deposits of southwestern Alaska (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1187)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 89 S. + 8 pl.
    Series Statement: U.S. Geological Survey bulletin 1187
    Language: English
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  • 19
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    Black Canyon of the Gunnison : today and yesterday (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1191)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VII, 76 S.
    Series Statement: U.S. Geological Survey bulletin 1191
    Language: English
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  • 20
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    Bibliography of reports resulting from U. S. Geological Survey participation in the United States technical assistance program, 1940 - 65 (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1193)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 51 S.
    Series Statement: U.S. Geological Survey bulletin 1193
    Language: English
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  • 21
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    Geologic reconnaissance along the Alaska Highway Delta River to Tok Junction, Alaska (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1181-H)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, H-19 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1181-H
    Language: English
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  • 22
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    Distribution of minor elements in coals of the Appalachian region (1966)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1117-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, C-37 S.
    Series Statement: U.S. Geological Survey bulletin 1117-C
    Language: English
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  • 23
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    Humate in coastal sands of northwest Florida (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1214-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, B-29 S.
    Series Statement: U.S. Geological Survey bulletin 1214-B
    Language: English
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  • 24
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    The Supai Group : subdivision and nomenclature (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1395-J)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, J-11 S.
    Series Statement: U.S. Geological Survey bulletin 1395-J
    Language: English
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  • 25
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    Geological and geophysical studies of chromite deposits in the Josephine Peridotite, northwestern California and southwestern Oregon (1984)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1546-A-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 86 S. + 5 pl.
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    Language: English
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  • 26
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    Feasibility and cost of using a computer to prepare landslide susceptibility maps of the San Francisco Bay Region, California (1978)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1443)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, 27 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1443
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  • 27
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    Mesozoic formations in the Comobabi and Roskruge Mountains, Papago Indian Reservation, Arizona (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1194-H)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, H-15 S.
    Series Statement: U.S. Geological Survey bulletin 1194-H
    Language: English
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  • 28
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    Chemical comparison of glassy and crystalline volcanic rocks (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1201-D)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, D-24 S.
    Series Statement: U.S. Geological Survey bulletin 1201-D
    Language: English
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  • 29
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    Lower Mesozoic extrusive rocks in southeastern Arizona - the Canelo Hills volcanics (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1194-M)
    In: U.S. Geological Survey bulletin
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    Pages: III, M-9 S.
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  • 30
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    Bauxite deposits of the Andersonville district Georgia (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1199-G)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, G-37 S. + 3 pl.
    Series Statement: U.S. Geological Survey bulletin 1199-G
    Language: English
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  • 31
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    Basic concepts of computerized digital image processing for geologists (1979)
    Washington, DC : United States Gov. Print. Off.
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    Call number: Sr 90.0001(1462)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 16 S. + 4 pl.
    Series Statement: U.S. Geological Survey bulletin 1462
    Language: English
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  • 32
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    Geology of the Puddle Springs quadrangle Fremont County, Wyoming (1967)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1242-C)
    In: U.S. Geological Survey bulletin
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    Pages: III, C-36 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1242-C
    Language: English
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  • 33
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    Biological aspects of terrestrial oil spills : USA CRREL oil research in Alaska, 1970-1974 ; [Final Report] (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-346
    In: Research report / Cold Regions Research and Engineering Laboratory, 346
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - USA CRREL project and personnel involvement. - Part I. Introduction. - Background. - Literature review. - Part II. CRREL investigations from 1970 - 1974. - Initial literature survey (1970). - Oil detection kit development. - Survey of Cape Simpson, Alaska, natural crude oil seepages (1970). - Haines-Fairbanks military pipeline investigations (1971-1973). - Barrow investigations (1970-1974). - Fairbanks and Fox investigations. - Germination studies. - Physiological studies. - Dispersant studies. - Microbiological investigations. - Field investigations of accidental petroleum losses. - Part III. Recent related literature. - Part IV. Conclusions and recommendations. - USA CRREL reports, publications and presentations on Alaska oil spill research. - Literature cited.
    Description / Table of Contents: Knowledge concerning the biological effects of oil pollution on arctic and subarctic terrestrial ecosystems is limited. USA CRREL research personnel conducted investigations from 1970 through 1974 to expand information in this field. Objectives were to: 1) define the ecosystems most sensitive to the presence of crude oil or its refined products, 2) quantify and understand the injury response, and 3) establish time frames for manifestation of damage and natural restorative processes in arctic and subarctic regions. This was accomplished through: 1) surveys of natural oil seepages and past accidential spills in the Arctic and Subarctic, 2) initiation of controlled oil spills and 3) detailed laboratory investigations. Results demonstrated that terrestrial oil spills will to some degree be detrimental to both arctic and subarctic plant communities. Degree and longevity of damage will be influenced primarily by the magnitude of the spill, season of occurrence and existing soil moisture content. Rapid recovery of plant communities subjected to spills will occur only if root systems remain relatively unaffected. Damage will be more extensive and long-term when root systems are saturated with oil. Effects of damage will be manifested gradually over several seasons being influenced by winter stresses. Variation does exist in plant species susceptibility. Carex aquatilis, a predominant sedge of the arctic, is markedly resistant to crude oil damage. In the taiga Picea mariana is very susceptible. Plant recovery can be enhanced through the application of fertilizer. Fertilization, in addition to its direct effect on plant nutrition, will stimulate microbial decomposition of crude oil.
    Type of Medium: Series available for loan
    Pages: vii, 66 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory 346
    URL: https://apps.dtic.mil/docs/citations/ADA047365
    Language: English
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  • 34
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    Isua, Greenland : glacier freezing study (1975)
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-334
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - List of symbols and associated dimensions. - Introduction and purpose. - Site characteristics. - Outline of study scheme. - Analysis. - Heat conduction to the drill hole. - Heat transfer between conduit wall and coolant. - Heat transfer between surface pipe and air. - Total heat extraction process. - Example calculations. - Estimate of basal water thickness and flow rates. - Summary of investigations of multiple-hole. - Literature cited.
    Description / Table of Contents: A scheme for cooling the lower portion of the edge of the Greenland ice sheet, which abuts a potential mining operation, is examined. The magnitude of cooling which may be accomplished by drilling a series of holes about the periphery of the mine site is determined as a function of hole size, spacing and time. Refrigeration is accomplished by pumping a coolant downhole in a central pipe, then uphole in an annulus between the pipe and hole wall, and then through a thin-walled pipe exposed to the surface climate above the ice sheet. It was found possible to achieve a temperature change in the ice of the order of -1°C with hole spacings and pumping requirements which are considered reasonable. Other effects are briefly examined and include an estimate of the basal water thickness and flow rates.
    Type of Medium: Series available for loan
    Pages: vii, 19 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 334
    URL: http://www.worldcat.org/oclc/227384248
    Language: English
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  • 35
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    Series available for loan
    Differential sea ice drift (1975)
    Hanover, NH : Corps of Engineers, U.S. Army, Cold Regions Research and Engineering Laboratory,
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    Call number: ZSP-202-329
    In: Research report
    Description / Table of Contents: CONTENTS: General Introduction. - Part I. Spatial and temporal variations in sea ice deformatfon. - Introduction. - Approach. - Site location and data collection procedures. - Data analysis. - Strain results. - Comparison of mesoscale deformation with macroscale deformation. - Nature of the ice pack rotation. - Conciusion. - Literature cited. - Part Il. Comparison of mesoscale strain measurements with linear drift theory predictions. - Introduction. - List of symbols. - Linear drift equations. - Ice drift solutions. - Comparison of theory with mesoscale measurements. - A more general linear constitutive law. - Conclusions. - Literature cited. - Appendix Relative magnitudes of differential drift forces. - Abstract.
    Description / Table of Contents: Measurements of mesoscale sea ice deformation over a region approximately 20 km in diameter were made over a five-week period in the spring of 1972 at the main AIDJEX camp in the Beaufort Sea. They have been analyzed to determine nonlinearities in the ice velocity field (due to the discrete small-scale nature of the ice pack), as well as a continuum mode of deformation represented by a least squares strain rate tensor and vorticity. The deformation rate time series between Julian day 88 and 113 exhibited net areal changes as large as 3% and deformation rates up to 0.16% per hour. In the principal axis coordinate system, the strain rate typically exhibited a much larger compression (or extension) along one axis than along the other. Persistent cycles at ~12-hour wavelengths were observed in the divergence rate. A comparison of the average residual error with the average strain rate magnitude indicated that strains measured on a scale of 10 km or greater can serve as a valid measure of the continuum motion of the sea ice. This conclusion is also substantiated by a comparison between the mesoscale deformation, and macroscale deformation measured over a ~100-km-diameter region. Vorticity calculations indicate that at low temporal frequencies ( 〈 0.04 hr^-1 ) the whole mesoscale array rotates essentially as an entity and consequently the low frequency vorticity can accurately be estimated from the rotation of a single floe. (Part I) A comparison of mesoscale strain measurements with the atmospheric pressure field and the wind velocity field indicated that the ice divergence rate and vorticity followed the local pressure and wind divergence with significant correlation. For low atmospheric pressures and converging winds, the divergence rate was negative with the vorticity being counterclockwise. The inverse behavior was observed for high pressures and diverging winds. This behavior agreed with predictions based upon the infinite boundary solution of a linearized drift theory in the absence of gradient current effects and using the constitutive law proposed by Glen for pack ice. The best least squares values of the constitutive law parameters [Eta] and [Zeta] were found to be given by ~10^12 kg sec^-1. Using typical divergence rates, these values yielded compressive stresses of the magnitude of 10^5 N m^-1, which are similar to values suggested by the Parmerter and Coon ridge model. In general, the infinite boundary solution of the linear drift equation indicates that in a low pressure region that is reasonably localized in space, the ice would be expected to converge for high compactness (winter) and diverge for low compactness (summer). Calculations were also carried out using a more general linear viscoelastic constitutive law that includes memory effects and that includes a generalized Hooke's law as well as the Glen law as special cases. A best fit of this more general calculation with strain measurements indicates, overall, a better agreement with viscous behavior than with elastic behavior, with the frequency behavior of the estimated "viscosities" similar to the Glen law behavior at temporal frequencies less than ~0.01 hr^-1 (Part II)
    Type of Medium: Series available for loan
    Pages: v, 37 Seiten , Illustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 329
    URL: http://www.worldcat.org/oclc/1387886
    Language: English
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  • 36
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    Analysis of hydrologic response to rain-on-snow (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-340
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Nomenclature. - Introduction. - Theory. - Application. - Literature cited. - Appendix.
    Description / Table of Contents: The equations describing water movement in a dry snow cover are derived and examples of flow through ripe, refrozen and fresh snows are given. The grain size of snow has a large effect on the timing of water discharge. Water is retained by dry snow to raise its temperature and satisfy the irreducible water saturation. These requirements delay and reduce runoff following rain on dry snow.
    Type of Medium: Series available for loan
    Pages: iv, 13 S. : graph. Darst.
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 340
    URL: https://usace.contentdm.oclc.org/digital/collection/p266001coll1/id/6127/rec/2
    Language: English
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  • 37
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    Gas inclusions in the Antarctic ice sheet and their significance (1975)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-339
    In: Research report
    Description / Table of Contents: CONTENTS: Abstract. - Preface. - Introduction. - Analytical procedures. - Thick section analysis. - Measurements of inclusion pressure. - Gas volume measurements. - Density and porosity measurements. - Results and discussion. - Sizes, shapes and distributions of bubbles. - Sizes, shapes and distributions of cavities. - Inclusion abundances. - Gas pressures in bubbles and cavities. - Total gas content. - Case for lattice diffusion. - Literature cited.
    Description / Table of Contents: Cores obtained to the bottom of the Antarctic Ice Sheet at Byrd Station were used to analyze the physical properties of air bubbles trapped in the ice. These bubbles originate as pockets of air in the upper layers of snow and approximately 10 ml of air/100 cm^3 of ice; i.e., 10% by volume is retained permanently when the snow transforms into ice. Parameters measured were the sizes, shapes, abundances, spatial distributions, gas volumes and pressures of bubbles, and their variations with depth in the ice sheet. Bubbles occur abundantly in the top 800 m of ice but then gradually disappear until they can no longer be detected optically below 1100 m. This disappearance is not accompanied by any significant loss of air from the ice and all available evidence indicates that the air actually diffuses into the ice in response to increasing overburden pressure. The possibility exists that the dissolved gases are retained in the form of a gas hydrate or clathrate which, because of release of confining pressures, begins to decompose soon after ice cores are pulled to the surface. This decomposition is accompanied by the growth of gas-filled bubble-like cavities, and as much as 40% of the dissolved air has exsolved already from some cores in the space of less than three years. Bubble pressure measurements show that 1) bubbles with pressures exceeding about 16 bars begin to relax back to this value soon after in situ pressures are relieved by drilling, 2) further slow decompression occurs with time, and 3) the rate of decompression is controlled to some extent by the intrinsic structural properties of the ice and its thermal and deformational history. Only small variations were observed in the entrapped air content of the ice cores; they probably reflect variations in the temperature and/or pressure of the air at the time of its entrapment, but the data are not sufficient to draw any firm conclusions regarding past variations in ice sheet thickness. Only ice from the bottom 4.83 m was found to lack any detectable trace of air. Since this absence of air coincided precisely with the first appearance of stratified moraine in the cores, it is concluded that this ice originated from the refreezing of air-depleted water produced under pressure melting conditions at the bottom of the ice sheet.
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    Pages: v, 18 Seiten , Illlustrationen
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 339
    URL: http://www.worldcat.org/oclc/1086574366
    Language: English
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  • 38
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    Stability of difference approximation to shock wave propagation in inhomogeneous elastic-plastic media (1969)
    Hanover, NH : Corps of Engineers, U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-202-277
    In: Research report
    Description / Table of Contents: CONTENTS: Preface. - Nomenclature. - Introduction. - Basic equations. - Constitutive relations. - Elastic region. - Plastic region. - Stability of the differential equation. - Stability of the difference equation. - Literature cited.
    Description / Table of Contents: An analysis is made of the stability of difference approximation to one-dimensional shock wave propagation in elastic-plastic media. The necessary condition for stability is obtained.
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    Pages: iv, 9 Seiten
    Series Statement: Research report / Cold Regions Research and Engineering Laboratory, CRREL, US Army Material Command 277
    URL: http://www.worldcat.org/oclc/5974046
    Language: English
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  • 39
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    Yeoloyikó chártis tís Elládhas 1:500 000 (1983)
    Stuttgart : Institute of Geology and Mineral Exploration
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    Call number: K 97.0014/1-2
    Pages: total 140x192, gef. cm
    Edition: 2nd ed.
    Language: English
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  • 40
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    International project on paleolimnology and late cenozoic climate (1979)
    Innsbruck : Univ.-Verl. Wagner ; Nachgewiesen 2.1979 -
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    Call number: ZSP-387
    Language: English
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  • 41
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    Carte tectonique internationale de l'Europe et des régions avoisinantes 1:2500 000 (1981)
    Moscou : Academy of Sciences of the USSR
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    Call number: K 93.0005/1-20
    Pages: je 91x71 cm
    Edition: 2nd ed.
    Language: English
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  • 42
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    Surficial geology of the Athol quadrangle Worcester and Franklin Counties, Massachusetts (1966)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1163-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, C-20 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1163-C
    Language: English
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  • 43
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    Geology of the Wayland quadrangle, Stephens and Eastland Counties, Texas (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1201-C)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, C-63 S. + 3 pl.
    Series Statement: U.S. Geological Survey bulletin 1201-C
    Language: English
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  • 44
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    Carbonate rocks of Cambrian and Ordovician age Northampton and Bucks Counties, eastern Pennsylvania and Warren and Hunterdon Counties, western New Jersey (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1194-L)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, L-7 S.
    Series Statement: U.S. Geological Survey bulletin 1194-L
    Language: English
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  • 45
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    Bedrock geology of the Grand Lake area Aroostook, Hancock Penobscot, and Washington Counties, Maine (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1201-E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, E-38 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1201-E
    Language: English
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  • 46
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    Geology of the Kayenta and Chilchinbito quadrangles Navajo County, Arizona (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1201-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, A-28 S. + 3 pl.
    Series Statement: U.S. Geological Survey bulletin 1202-A
    Language: English
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  • 47
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    Nomenclature and correlation of lithologic subdivisions of the Jefferson and Three Forks Formations of southern Montana and northern Wyoming (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1194-N)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, N-18 S.
    Series Statement: U.S. Geological Survey bulletin 1194-N
    Language: English
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  • 48
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    Measurement of the remanent magnetization of igneous rocks (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1203-A)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, A-32 S.
    Series Statement: U.S. Geological Survey bulletin 1203-A
    Language: English
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  • 49
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    Structural dislocations in eastern Massachusetts (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1410)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 39 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1410
    Language: English
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  • 50
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    A summary of oil and gas production and reserve histories of the Appalachian basin, 1859-1972 (1975)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1409)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, 36 S.
    Series Statement: U.S. Geological Survey bulletin 1409
    Language: English
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  • 51
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    The Matagamon Sandstone - a new Devonian formation in north-central Maine (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1194-F)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, F-9 S.
    Series Statement: U.S. Geological Survey bulletin 1194-F
    Language: English
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  • 52
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    Mesozoic formations in the Vekol Mountains Papago Indian Reservation Arizona (1965)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1194-G)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, G-9 S.
    Series Statement: U.S. Geological Survey bulletin 1194-G
    Language: English
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  • 53
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    Geology and mineral deposits of the Needle Mountains district, southwestern Colorado (1977)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1434)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: VI, 40 S. + 1 pl.
    Series Statement: U.S. Geological Survey bulletin 1434
    Language: English
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  • 54
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    Stratigraphy, preliminary petrology, and some structural features of Tertiary volcanic rocks in the Gabbs Valley and Gillis Ranges, Mineral County, Nevada (1980)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1464)
    In: U.S. Geological Survey bulletin
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    Pages: IV, 54 S.
    Series Statement: U.S. Geological Survey bulletin 1464
    Language: English
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  • 55
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    Geology of the Garns Mountain quadrangle Bonneville, Madison, and Teton Counties, Idaho (1966)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1205)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: V, 122 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1205
    Language: English
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  • 56
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    Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1975 (1976)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1222-A)
    In: U.S. Geological Survey bulletin
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    Pages: III, A-84 S.
    Series Statement: U.S. Geological Survey bulletin 1422-A
    Language: English
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  • 57
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    Geology of the northwest quarter of the Anaconda quadrangle Deer Lodge County, Montana (1966)
    Washington, DC : United States Gov. Print. Off.
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    Call number: SR 90.0001(1222-B)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: III, B-28 S. + 2 pl.
    Series Statement: U.S. Geological Survey bulletin 1222-B
    Language: English
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  • 58
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    General climatology (1976)
    Warszawa : Polish Scient. Publ.
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    Call number: PIK N 456-11-0194
    Description / Table of Contents: Contents: 1. Climatology as a science ; 2. Climate-forming factors ; 3. Geographical distribution and variation of major meteorological elements ; 4. A brief survey of major types of climate ; 5. Changes and fluctuations of climates
    Type of Medium: Monograph available for loan
    Pages: XIV, 422 S. : graph. Darst., 1 Kt.
    Uniform Title: Klimatologia ogólna
    Language: English
    Location: A 18 - must be ordered
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  • 59
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    Effect of temperature on strength of snow-ice (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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
    URL: https://apps.dtic.mil/dtic/tr/fulltext/u2/a067583.pdf
    Language: English
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  • 60
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    Performance of the St. Marys River ice booms, 1976-1977 (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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
    URL: https://hdl.handle.net/11681/9383
    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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  • 61
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    Ice fog suppression using reinforced thin chemical films (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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.
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    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 78-26
    URL: https://hdl.handle.net/11681/9456
    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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  • 62
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    Nondestructive testing of in-service highway pavements in Maine (1979)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-79/6
    In: CRREL Report, 79-6
    Description / Table of Contents: Nondestructive repetitive plate bearing (RPB) tests were conducted on various test sections in state highways in Maine during 13-15 April 1976. The RPB test consists of making resilient surface deflection measurements during repetitive loadings at various radii from the load plate. The pavement system stiffness was calculated and the resilient modulus values for the various pavement layers were determined with the Chevron computer program for a layered elastic system. A thawed analysis using nondimensional deflection curves for the various sections provided a guide to the susceptibility of the pavement systems to surface failure and pothole development. Some comparisons between stabilized and nonstabilized aggregate and soil were made with calculated stiffness values. The moduli of the various materials were also compared. The residual surface deflections during testing for several pavement systems indicated a linear logarithmic relationship with number of load applications. A relationship between the modulus of the asphalt cement concrete pavement and pavement temperature was developed for the limited temperature range during the testing.
    Type of Medium: Series available for loan
    Pages: v, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 79-6
    URL: https://hdl.handle.net/11681/9013
    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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  • 63
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    Penetration tests in subsea permafrost, Prudhoe Bay, Alaska (1979)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-79/7
    In: CRREL Report, 79-7
    Description / Table of Contents: Sediments beneath the Beaufort Sea near Prudhoe Bay, Alaska, were probed at 27 sites using a static cone penetrometer to determine engineering properties and distribution of material types, including ice-bonded sediments. The probe provided both point and casing resistance data and thermal profiles. At five sites these data were correlated with information from adjacent drilled and sampled holes. These control data and the quality of the probe information permitted profiles of sediment type and occurrence of ice-bonded material to be developed along three lines that included various geological features and depositional environments. Material properties were quite variable in the upper 14 m of sediments probed. In general, softer, finer-grained sediments occurred in the upper layers, while penetration refusal was met in stiff gravels to 10 to 12 m below the seabed. Seabed temperatures during the study were all below 0 C. However, because of uncertainties in freezing point values caused by brines, evaluation of the penetration resistance data was required to identify the occurrence of ice-bonded sediments. The coupling of thermal and penetration resistance data revealed that seasonally ice-bonded sediments occurred where the sea ice froze back to or near the seabed. Deeper, perennially frozen sediments also appeared to be present at several probe sites. The penetration data obtained can be used to aid in the design of shallow and deep foundations in both ice-bonded and unfrozen subsea sediments.
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    Pages: iv, 49 Seiten , Illustrationen
    Series Statement: CRREL Report 79-7
    URL: https://hdl.handle.net/11681/9014
    Language: English
    Note: CONTENTS Abstract Preface Introduction Equipment Data collection and reduction Data analysis and interpretation Point penetration resistance and material properties Lithologic and temperature profiles Casing penetration resistance Applications Shallow foundations Deep foundations Foundations in permafrost Correlations with laboratory tests Conclusions Selected bibliography Appendix A: Description of penetrometer and test procedures Appendix B: Point resistance and skin friction data
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  • 64
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    Segregation freezing as the cause of suction force for ice lens formation (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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
    URL: https://hdl.handle.net/11681/9411
    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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  • 65
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    Interaction of a surface wave with a dielectric slab discontinuity (1978)
    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
    URL: https://hdl.handle.net/11681/9408
    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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  • 66
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    Measurement and identification of aerosols collected near Barrow, Alaska (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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
    URL: https://hdl.handle.net/11681/9391
    Language: English
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  • 67
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    Primary production in sea ice of the Weddell region (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    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
    URL: https://hdl.handle.net/11681/9389
    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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  • 68
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    Shoreline changes along the outer shore of Cape Cod from Long Point to Monomoy Point (1978)
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-78/17
    In: CRREL Report, 78-17
    Description / Table of Contents: Abstract: This investigation utilized historical and recent aerial photographs and satellite imagery in 1) estimating changes in positions of the high-water line and sea cliff break and base, in rates of accretion and/or erosion, and in volumes of transported sediment, and 2) providing a preliminary evaluation of the direction of littoral transport along the outer Cape Cod coast. Using aerial photographs acquired in 1938, 1952, 1971 and 1974 with manual photointerpretation techniques, changes in the distances from selected reference points to the cliff break, cliff base and the high-water line were measured. LANDSAT-1 and -2 imagery acquired from 1 September 1972 to 28 May 1975 was evaluated for use in determining the directions of littoral transport that are active the predominant amount of time. Although the imagery has been very useful for this purpose at other locations, it proved to be useless along the outer shore of Cape Cod. Largest net migrations of the high water line from 1938 to 1974 occurred in the northern and southern portions of this coast. The northern maximum high water line was 321.4 ft, the southern was 1794.6 ft. The central portion of the coast was generally more stable with changes varying from 6.8 to 157.6 ft. Cliff-base recession rates varied from 0.4 to 7.3 ft/yr. Maximum estimated net volume of sediment deposited per linear foot of beach from 1938 to 1974 was 334 yd^3 (based on 2 yd^3/ft of recession or accretion); maximum eroded was 914 yd^3. Changes in the configuration of spits were used to evaluate directions of littoral transport since suspended sediment concentrations were generally not sufficient to act as natural tracers of surface currents. Based on the literature and a determination of the portion of the coast perpendicular to the direction of dominant wave approach, the location of the nodal zone for predominant littoral directions of drift probably shifts between the area near Spectacle Pond and North Truro Air Force Station. This investigation has illustrated a photo interpretation technique that is useful in performing a reconnaissance of coastal change. The data obtained from this method can be used to supplement those acquired by ground surveys and are valid as first approximations for planning subsequent, more detailed surveys.
    Type of Medium: Series available for loan
    Pages: vi, 49 Seiten , Illustrationen
    Series Statement: CRREL Report 78-17
    URL: https://hdl.handle.net/11681/9394
    Language: English
    Note: CONTENTS Abstract Preface Conversion factors: U.S. customary to metric units of measurement Introduction Background Previous investigations Analytical procedures Results and discussion Shoreline changes: High-water line Shoreline changes: Cliff recession Volumetric changes Nodal zone location and direction of littoral transport Error evaluation Summary and conclusions Future research Selected bibliography Appendix A: Maps of shoreline with overlays for 1938, 1952, 1971 and 1974 Appendix B: Supplementary data for estimating shoreline change
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  • 69
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    Stress and strain : basic concepts of continuum mechanics for geologists (1976)
    New York [u.a.] : Springer
    Details Availability
    Call number: 9/M 92.0755 ; O 8668 ; 11374
    Type of Medium: Monograph available for loan
    Pages: xi, 339 S.
    ISBN: 0387075569
    Classification:
    Tectonics
    Language: English
    Location: Reading room
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  • 70
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    Makroseismic intensities observed in Czechoslovakia and Poland = Makrosejsmiczne intensywnosci w czechoslowacji i Polsce (1978)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-3) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 75 S.
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 3 = 122
    Language: English
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  • 71
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    Results of geomagnetic observations Belsk 1975 (1976)
    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(C-2) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 55 S.
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : C, Geomagnetism 2 = 107
    Language: English
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  • 72
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    Petroleum formation and occurrence : a new approach to oil and gas exploration (1978)
    Berlin [u.a.] : Springer
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    Call number: G 7638
    Type of Medium: Monograph available for loan
    Pages: XVIII, 538 S.
    ISBN: 3540086986
    Language: English
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  • 73
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    Phase transitions in iron oxides and sulphides and their relations to magnetic properties of rocks (1983)
    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(C-15) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 92 S.
    ISBN: 830104330X
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : C, Geomagnetism 15 = 164
    Language: English
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  • 74
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    Selected papers on data analysis and numerical methods in geophysics 1976 (1977)
    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(G-1) / Rgal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 54 S.
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : G, Numerical methods in geophysics 1 = 110
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  • 75
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    Seismological bulletin 1980, part 1 : January, February, March (1981)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-7,1) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
    Type of Medium: Series available for loan
    Pages: 50 S.
    ISBN: 8301040157
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : B, Seismology 7 = 161
    Language: English
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    Hydraulic fracturing and geothermal energy : proceedings of the First Japan-United States Joint Seminar on Hydraulic Fracturing and Geothermal Energy, Tokyo, Japan, November 2 - 5, 1982, and Symposium on Fracture Mechanics Approach to Hydraulic Fracturing and Geothermal Energy, Sendai, Japan, November 8 - 9, 1982 (1983)
    Dordrecht [u.a.] : Nijhoff
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    In: Mechanics of elastic stability
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    Pages: XI, 528 S.
    ISBN: 902472855X
    Series Statement: Mechanics of elastic and inelastic solids 5
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    Continental networks : report on the activities of the IAG-Commission X 1979 to 1983 (1984)
    München : Beck
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    Call number: SR 99.0125(266)
    In: Deutsche Geodätische Kommission bei der Bayerischen Akademie der Wissenschaften
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    Pages: 48 S.
    ISBN: 3769685598
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    Factors Controlling the Clay Mineralogy of Egyptian Phanerozoic Mudrocks and Marls (1983)
    Hannover : Schweizerbart
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    Call number: SR 99.0054(49)
    In: Geologisches Jahrbuch
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    Climates throughout geologic time (1979)
    Amsterdam [u.a.] : Elsevier
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    Pages: XII, 310 S. : Abb.
    ISBN: 044441925x
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    Seismological bulletin 1979, part 4 : October, November, December (1981)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-6,4) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 172 S.
    ISBN: 8301038829
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    Seismological bulletin 1979, part 1 : January, February, March (1980)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-6,1) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 45 S.
    ISBN: 8301030100
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    Bulletin séismologique 1976, part 5 : les secousses locales enregistrées par les stations séismologique polonaises (1979)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-2,5) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 252 S.
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    Directory of institutions : active in research in mineralogy, petrology, geochemistry and their applications (1982)
    Società Italiana di Mineralogia e Petrologia
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    Pages: 32 S.
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    Bulletin séismologique 1976, part 1 : janvier, février, mars (1977)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Bulletin séismologique 1975, part 3 : juillet, aout, septembre (1976)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-1,3) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 136 S.
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    Results of geomagnetic observations Hel Geophysical Observatory 1971-1975 (1979)
    Warszawa : Panstw. Wyd. Naukowe
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    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 248 S.
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    Results of geomagnetic observations Belsk 1978 (1979)
    Warszawa : Panstw. Wyd. Naukowe
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    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Results of geomagnetic observations Hel Geophysical Observatory 1966-1970 (1979)
    Warszawa : Panstw. Wyd. Naukowe
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    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 266 S.
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    Results of geomagnetic observations Belsk 1976 (1977)
    Warszawa : Panstw. Wyd. Naukowe
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    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Results of geomagnetic observations Belsk 1977 (1978)
    Warszawa : Panstw. Wyd. Naukowe
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    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Earth tides May 1981 - May 1982 = Marées terrestres Mai 1981 - Mai 1982 (1983)
    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(F-10) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 75 S.
    ISBN: 8301054824
    Series Statement: Publications of the Institute of Geophysics, Polish Academy of Sciences : F, Planetary geodesy 10 = 172
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    Results of geomagnetic observations Belsk 1983 (1984)
    Warszawa : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(C-20) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 75 S.
    ISBN: 8301061332
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    Monitoring underground nuclear explosions (1977)
    Amsterdam [u.a.] : Elsevier
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    Call number: 10211
    Type of Medium: Monograph available for loan
    Pages: X, 440 S.
    ISBN: 0444416048
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    Multichannel time series analysis : with digital computer programs (1983)
    Houston, Texas : Goose Pond Pr.
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    Call number: O 5900 ; MOP 19237
    Type of Medium: Monograph available for loan
    Pages: xxvii, 454 S.
    Edition: 2nd ed.
    ISBN: 0910835039
    Language: English
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    The chemical evolution of the atmosphere and oceans (1984)
    Princeton : Princeton Univ. Pr.
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    Call number: 10/M 92.1066 ; M 93.0029 ; PIK N 454-94-0391
    Type of Medium: Monograph available for loan
    Pages: xii, 582 S.
    ISBN: 0691083487
    Series Statement: Princeton series in geochemistry
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    Seismological bulletin 1979, part 2 : April, May, June (1981)
    Warszawa [u.a.] : Panstw. Wyd. Naukowe
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    Call number: SR 91.0236(B-6,2) / Regal 35
    In: Publications of the Institute of Geophysics, Polish Academy of Sciences
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    Pages: 97 S.
    ISBN: 8301034785
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    Metal deposits in relation to plate tectonics (1984)
    Berlin [u.a.] : Springer
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    Call number: G 8431 ; 10/M 93.0092/17
    In: Minerals and rocks
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    Pages: XIV, 325 S.
    ISBN: 3540127526
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    Plate tectonics and crustal evolution (1982)
    New York [u.a.] : Pergamon Press
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    Call number: M 377
    Type of Medium: Monograph available for loan
    Pages: IX, 310 S. : Ill.
    Edition: 2. ed.
    ISBN: 0080280765
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    Ophiolites and oceanic lithosphere (1979)
    Oxford : Blackwell Scientific Publications
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    Call number: 9/G 9202
    In: Special publications / the Geological Society, London, Volume 13
    Description / Table of Contents: Preface The proposal that ophiolites are on-land fragments of oceanic lithosphere has been with us for over 20 years and has been widely accepted by the Earth Sciences' community. Despite this, many oceanographers are reluctant to use ophiolite data. Their argument (and it comes largely from the geological rather than geophysical oceanographers) is that 'Even if ophiolites are on-land fragments of oceanic lithosphere, they must be atypical for otherwise they would have been subducted and not obducted'. So they conclude that, although the study of ophiolites is perfectly acceptable in its own right, its results should not be used in the investigation of present-day, in-situ oceanic lithosphere--i.e, the invoking of 'reversed uniformitarianism' is not acceptable. However using uniformitarian principles to interpret ophiolites from present-day oceanic lithosphere studies is equally problematical for (i) petrological/geochemical studies of ocean-floor rocks are based on widely spaced boreholes of limited depth and dredge-haul sampling, (ii) geophysical data can only detect large-scale phenomena and are open to various interpretations, and (iii) direct observations from submersibles are still very limited. Such circumstances should have drawn the two groups of workers closer together.
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    Pages: VI, 413 Seiten , Illustrationen
    ISBN: 0632012196
    Series Statement: Special publications / the Geological Society, Londonn 13
    URL: https://doi.org/10.1144/GSL.SP.1984.013.01.01
    Language: English
    Note: I. Nature and Formation of Oceanic Lithosphere --- Magma Chambers: Products and Processes --- J. A. Orcutt, M. Burnett, and J. S. McClain: Evolution of the ocean crust: results from recent seismic experiments / Geological Society, London, Special Publications, 13:7-16, doi:10.1144/GSL.SP.1984.013.01.01 --- M. R. Fisk: Depths and temperatures of mid-ocean-ridge magma chambers and the composition of their source magmas / Geological Society, London, Special Publications, 13:17-23, doi:10.1144/GSL.SP.1984.013.01.02 --- M. F. J. Flower: Spreading-rate parameters in ocean crust: analogue for ophiolite? / Geological Society, London, Special Publications, 13:25-40, doi:10.1144/GSL.SP.1984.013.01.03 --- J. D. Smewing, N. I. Christensen, I. D. Bartholomew, and P. Browning: The structure of the oceanic upper mantle and lower crust as deduced from the northern section of the Oman ophiolite / Geological Society, London, Special Publications, 13:41-53, doi:10.1144/GSL.SP.1984.013.01.04 --- R. T. Gregory: Melt percolation beneath a spreading ridge: evidence from the Semail peridotite, Oman / Geological Society, London, Special Publications, 13:55-62, doi:10.1144/GSL.SP.1984.013.01.05 --- J. S. Pallister: Parent magmas of the Semail ophiolite, Oman / Geological Society, London, Special Publications, 13:63-70, doi:10.1144/GSL.SP.1984.013.01.06 --- P. Browning: Cryptic variation within the Cumulate Sequence of the Oman ophiolite: magma chamber depth and petrological implications / Geological Society, London, Special Publications, 13:71-82, doi:10.1144/GSL.SP.1984.013.01.07 --- D. Elthon, J. F. Casey, and S. Komor: Cryptic mineral-chemistry variations in a detailed traverse through the cumulate ultramafic rocks of the North Arm Mountain massif of the Bay of Islands ophiolite, Newfoundland / Geological Society, London, Special Publications, 13:83-97, doi:10.1144/GSL.SP.1984.013.01.08 --- Fracture Zones --- R. S. White: Atlantic oceanic crust: seismic structure of a slow-spreading ridge / Geological Society, London, Special Publications, 13:101-111, doi:10.1144/GSL.SP.1984.013.01.09 --- J. M. Auzende, G. Ceuleneer, G. Cornen, T. Juteau, Y. Lagabrielle, G. Lensch, C. Mevel, A. Nicolas, H. Prichard, A. Ribeiro, E. Ruellan, and J. R. Vanney: Intraoceanic tectonism on the Gorringe Bank: observations by submersible / Geological Society, London, Special Publications, 13:113-120, doi:10.1144/GSL.SP.1984.013.01.10 --- J. Honnorez, C. Mevel, and R. Montigny: Occurrence and significance of gneissic amphibolites in the Vema fracture zone, equatorial Mid-Atlantic Ridge / Geological Society, London, Special Publications, 13:121-130, doi:10.1144/GSL.SP.1984.013.01.11 --- J. A. Karson: Variations in structure and petrology in the Coastal Complex, Newfoundland: anatomy of an oceanic fracture zone / Geological Society, London, Special Publications, 13:131-144, doi:10.1144/GSL.SP.1984.013.01.12 --- Mantle Structures --- A. Nicolas and M. Rabinowicz: Mantle flow pattern at oceanic spreading centres: relation with ophiolitic and oceanic structures / Geological Society, London, Special Publications, 13:147-151, doi:10.1144/GSL.SP.1984.013.01.13 --- Lavas and Sediments --- J. Malpas and G. Langdon: Petrology of the Upper Pillow Lava suite, Troodos ophiolite, Cyprus / Geological Society, London, Special Publications, 13:155-167, doi:10.1144/GSL.SP.1984.013.01.14 --- J. F. Boyle and A. H. F. Robertson: Evolving metallogenesis at the Troodos spreading axis / Geological Society, London, Special Publications, 13:169-181, doi:10.1144/GSL.SP.1984.013.01.1--- Isotope Studies & Metamorphism --- D. Elthon, J. R. Lawrence, R. E. Hanson, and C. Stern: Modelling of oxygen-isotope data from the Sarmiento ophiolite complex, Chile / Geological Society, London, Special Publications, 13:185-197, doi:10.1144/GSL.SP.1984.013.01.16 --- D. S. Stakes, H. P. Taylor , jr, and R. L. Fisher: Oxygen-isotope and geochemical characterization of hydrothermal alteration in ophiolite complexes and modern oceanic crust / Geological Society, London, Special Publications, 13:199-214, doi:10.1144/GSL.SP.1984.013.01.17 --- M. J. Thirlwall and B. J. Bluck: Sr-Nd isotope and chemical evidence that the Ballantrae ‘ophiolite’, SW Scotland, is polygenetic / Geological Society, London, Special Publications, 13:215-230, doi:10.1144/GSL.SP.1984.013.01.18 --- M. A. Menzies: Chemical and isotopic heterogeneities in orogenic and ophiolitic peridotites / Geological Society, London, Special Publications, 13:231-240, doi:10.1144/GSL.SP.1984.013.01.19 --- Zulfiqar Ahmed and A. Hall: Petrology and mineralization of the Sakhakot-Qila ophiolite, Pakistan / Geological Society, London, Special Publications, 13:241-252, doi:10.1144/GSL.SP.1984.013.01.20 --- II. Emplacement (Obduction) of Ophiolites --- Ophiolite Emplacement and Obduction --- J. G. Spray: Possible causes and consequences of upper mantle decoupling and ophiolite displacement / Geological Society, London, Special Publications, 13:255-268, doi:10.1144/GSL.SP.1984.013.01.21 --- J. F. Casey and J. F Dewey: Initiation of subduction zones along transform and accreting plate boundaries, triple-junction evolution, and forearc spreading centres—implications for ophiolitic geology and obduction / Geological Society, London, Special Publications, 13:269-290, doi:10.1144/GSL.SP.1984.013.01.22 --- Y. Ogawa and J. Naka: Emplacement of ophiolitic rocks in forearc areas: Examples from central Japan and Izu-Mariana-Yap island arc system / Geological Society, London, Special Publications, 13:291-301, doi:10.1144/GSL.SP.1984.013.01.23 --- M. P. Searle and R. K. Stevens: Obduction processes in ancient, modern and future ophiolites / Geological Society, London, Special Publications, 13:303-319, doi:10.1144/GSL.SP.1984.013.01.24 --- N. H. Woodcock and A. H. F. Robertson: The structural variety in Tethyan ophiolite terrains / Geological Society, London, Special Publications, 13:321-330, doi:10.1144/GSL.SP.1984.013.01.25 --- Regional Studies --- H. Colley: An ophiolite suite in Fiji? / Geological Society, London, Special Publications, 13:333-340, doi:10.1144/GSL.SP.1984.013.01.26 --- H. L. Davies and A. L. Jaques: Emplacement of ophiolite in Papua New Guinea / Geological Society, London, Special Publications, 13:341-349, doi:10.1144/GSL.SP.1984.013.01.27 --- J. S. Milsom: The gravity field of the Marum ophiolite complex, Papua New Guinea / Geological Society, London, Special Publications, 13:351-357, doi:10.1144/GSL.SP.1984.013.01.28 --- R. G. Coleman: Ophiolites and the tectonic evolution of the Arabian Peninsula / Geological Society, London, Special Publications, 13:359-366, doi:10.1144/GSL.SP.1984.013.01.29 --- G. Wadge, G. Draper, and J. F. Lewis: Ophiolites of the northern Caribbean: A reappraisal of their roles in the evolution of the Caribbean plate boundary / Geological Society, London, Special Publications, 13:367-380, doi:10.1144/GSL.SP.1984.013.01.30 --- B. A. Sturt, H. Furnes, and D. Roberts: A conspectus of Scandinavian Caledonian ophiolites / Geological Society, London, Special Publications, 13:381-391, doi:10.1144/GSL.SP.1984.013.01.31 --- R. Hall: Ophiolites: Figments of Oceanic Lithosphere? / Geological Society, London, Special Publications, 13:393-403, doi:10.1144/GSL.SP.1984.013.01.32 --- D. A. Rothery: The role of Landsat Multispectral Scanner (MSS) imagery in mapping the Oman ophiolite / Geological Society, London, Special Publications, 13:405-413, doi:10.1144/GSL.SP.1984.013.01.33
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    Monograph available for loan
    Introduction to geochemistry (1983)
    Auckland [u.a.] : McGraw-Hill
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    Call number: M 93.0216
    Type of Medium: Monograph available for loan
    Pages: XIII, 617 S. : graph. Darst.
    Edition: 2. ed., 2. print.
    ISBN: 0070354472
    Series Statement: McGraw-Hill international series in the earth and planetary sciences
    Language: English
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