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Collection
Years
Year
  • 1
    Series available for loan
    Series available for loan
    Stuttgart : Schweizerbart
    Associated volumes
    Call number: SR 90.0066(33)
    In: Geologisches Jahrbuch . Reihe A, Allgemeine und regionale Geologie Bundesrepublik Deutschland und Nachbargebiete, Tektonik, Stratigraphie, Paläontologie, 33
    Type of Medium: Series available for loan
    Pages: 159 S. , Ill., graph. Darst., Kt. , 2 Beil.
    Series Statement: Geologisches Jahrbuch / A Heft 33
    Language: German , English , French , Russian
    Note: Mit engl., franz. und russ. Zsfassungen
    Location: Lower compact magazine
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  • 2
    Call number: ZSP-SCAR-570-1
    In: Report to SCAR on Antarctic research activities of Germany (FRG), 1
    Type of Medium: Series available for loan
    Pages: 21 Seiten
    ISSN: 0179-0072
    Series Statement: Report to SCAR on Antarctic research activities of Germany (FRG) 1
    Language: English
    Note: Contents: Membership of the National Committee on Antarctic Research of the Federal Republic of Germany. - Introduction. - Station. - Field Activities 1974-1979. - Planned Activities 1979/80. - References.
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  • 3
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: MOP 40046 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 113 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
    Location: MOP - must be ordered
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  • 4
    Call number: ZSP-201-76/33
    In: CRREL Report, 76-33
    In: Detecting structural heat losses with mobile infrared thermography / R.H. Munis, S.J. Marshall and M.A. Bush, Part IV
    Description / Table of Contents: During the winter of 1973-74 a mobile infrared thermography system was used to survey campus buildings at Dartmouth College, Hanover, New Hampshire. Both qualitative and quantitative data are presented regarding heat flow through a small area of a wall of one brick dormitory building before and after installation of aluminum reflectors between radiators and the wall. These data were used to estimate annual cost savings for 22 buildings of similar construction having aluminum reflectors installed behind 1100 radiators. The data were then compared with the actual savings which were calculated from condensate meter data. The discrepancy between estimated and actual annual cost savings is explained in detail along with all assumptions required for these calculations.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 76-33
    Language: English
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  • 5
    Call number: MOP 41424 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 31 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 6
    Call number: MOP 44901 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 218 Seiten
    Edition: 19., völlig überarbeitete Auflage
    Language: German
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  • 7
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/13
    In: CRREL Report, 79-13
    Description / Table of Contents: Heat transfer in turbulent flow was measured in a rectangular channel with a width of 0.254 m and a flow depth of 0.0254 m. Correlations between the Nusselt and Reynolds numbers are given for a range of 3020 Re 22360. A Prandtl number range of 9.90 or = Pr or = 12.28 for water was used in the tests. The results are compared with those of other investigations and show that some well-known correlations underpredict the heat transfer by about 35%.
    Type of Medium: Series available for loan
    Pages: ii, 5 Seiten , Illustrationen
    Series Statement: CRREL Report 79-13
    Language: English
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  • 8
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/10
    In: CRREL Report, 79-10
    Description / Table of Contents: Ice cores from Byrd Station and Little America V have been used to test an ultrasonic technique for evaluating crystal anisotropy in the Antarctic Ice Sheet. P-wave velocities measured parallel and perpendicular to the vertical axes of cores from the 2164-m-thick ice sheet at Byrd Station have yielded results in excellent agreement with the observed c-axis fabric profile and with the in-situ P-wave velocity profile measured parallel to the bore hole axis. Velocity differences in excess of 140 m/s for core samples from deeper than 1300 m attest to the strong single pole clustering of crystallographic c-axes about the vertical, especially in the zone from 1300-1800 m. Such oriented structure is compatible only with strong horizontal shearing in this zone. The existence in an ice sheet of widespread shearing several hundred meters above its bed raises serious questions as to the validity of current concepts of the flow of large ice masses that tend to gloss over or ignore crystal alignments of this magnitude.
    Type of Medium: Series available for loan
    Pages: IV, 16 Seiten , Illustrationen
    Series Statement: CRREL Report 79-10
    Language: English
    Note: CONTENTS Abstract Preface Introduction Laboratory measurements Sample sources Ultrasonic velocity measurements Effects of inclined drilling at Byrd Station Results Byrd Station Little America V Summary and conclusions Literature cited
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  • 9
    Call number: ZSP-201-76/24
    In: CRREL Report, 76-24
    Description / Table of Contents: Chemical analysis of surface snows and deeper ice core samples from Milcent, Greenland, indicates a marine origin for Na and Cl and a terrestrial origin for Al, Mn and V. Pre-1900 enrichment factors, based on average crustal composition, are high for Zn and Hg and appear to be related to their volatility. A comparison of pre-1900 and 1971-1973 concentrations of V and Hg shows no decided increase from industrial production; however, the abundance of Zn (relative to Al) increased three-fold during this time period. The chemical composition of ancient ice is extremely useful in interpreting modern aerosols.
    Type of Medium: Series available for loan
    Pages: ii, 6 Seiten , Illustrationen
    Series Statement: CRREL Report 76-24
    Language: English
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  • 10
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/25
    In: CRREL Report, 76-25
    Description / Table of Contents: The primary objective of this investigation was to compile baseline information pertaining to the ocean circulation, especially the extent and patterns of tidal currents and tidal flushing, in Cook Inlet, Alaska, utilizing aircraft and satellite imagery with corroborative ground truth data. LANDSAT-1 and NOAA-2 and -3 imagery provided repetitive, synoptic views of surface currents, water mass migration and sediment distribution during different seasons and tides. Color, color infrared and thermal infrared imagery acquired on 22 July 1972 with the NASA NP-3A aircraft were used to analyze currents, mixing patterns and sediment dispersion in selected areas. Temperature(C), salinity (0/00) and suspended sediment concentration (mg/l) data and hand-held photography were utilized as ground truth information in the interpretation of the aircraft and satellite imagery. Coriolis effect, semidiurnal tides and the Alaska current govern the estuary circulation. Clear, oceanic water enters the inlet on the southeast during flood tide, progresses northward along the east shore with minor lateral mixing, and remains a distinct water mass to the latitude of Kasilof-Ninilchik. South of the forelands, mixing with turbid inlet water becomes extensive. Turbid water moves south primarily along the north shore during ebb tide and a shear zone between the two water masses forms in mid-inlet south of Kalgin Island. Currents adjacent to and north of the forelands are complicated by tidal action, coastal configuration and bottom effects. Turbulence is greatest throughout the water column along the south shore and stratification is more pronounced in Kamishak and Kachemak Bays, especially when fresh water runoff is high.
    Type of Medium: Series available for loan
    Pages: ix, 92 Seiten , Illustrationen
    Series Statement: CRREL Report 76-25
    Language: English
    Note: CONTENTS Abstract Preface Summary Conversion factors: U.S. customary to metric (SI) units of measurement. Introduction Background Objectives Project history Approach Aircraft imagery LANDSAT-1 imagery NOAA-2 and -3 satellite imagery Ground truth data Imagery and ground truth data analysis Physical and cultural setting Geography Geology Climate Hydrology Local industry and population density Sources of estuarine pollution Results and discussion Coastal configuration Bathymetry Tides Asymmetry of tidal flow/duration across inlet Suspended sediment distribution and circulation Sea ice Tidal flushing characteristics Summary and conclusions Applications Recommendations Literature cited Appendix A. RS-14 infrared scanner imagery
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  • 11
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/28
    In: CRREL Report, 76-28
    Description / Table of Contents: Fourier transforms of selected ground-motion time histories from five underground high-explosive and nuclear detonations are used to define the transmission properties (Transfer functions) of three rock types. Absorption, a measure of a rock's energy dissipating characteristics, is expressed for each of the tests as a function of the frequency of transmission. Dispersion results from a variation in transmission velocity with frequency and is described for each test by a phase velocity spectrum. The transmission properties from one of the sites are used to predict a ground-motion time history at that site from another nuclear event. The potential use of Fourier techniques to make ground-motion predictions and to measure in-situ material properties is discussed.
    Type of Medium: Series available for loan
    Pages: vi, 91 Seiten , Illustrationen
    Series Statement: CRREL Report 76-28
    Language: English
    Note: Contents Section I: Introduction Section II: Analytical procedures 1. Fourier transforms 2. Basic transform properties 3. Transform techniques 4. The transfer function Section II: Parameter studies and program evaluations 1. Analytical parameter study 2. I-TRAIN evaluation 3. S-TRAIN evaluation Section IV: Data 1. DATEX I 2. DATEX II 3. STARMET 4. MINERAL LODE 5. HARD HAT and PILEDRIVER Section V: Analysis of transformed data 1. Absorption 2. Dispersion 3. Transfer function Section VI: Fourier synthesis Section VII: Discussion Literature cited Appendix A: The Fourier integral and series Appendix B: Subroutine FOURT used in analysis Appendix C: I-TRAIN and S-TRAIN programs
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  • 12
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/32
    In: CRREL Report, 76-31
    Description / Table of Contents: Four large grounded multi-year shear ridge formations were found in the grounded ice subzone of the fast ice zone near the Harrison Bay/Prudhoe Bay area of Alaska. A 166-m-long cross section of one of these formations was obtained by leveling and sonar measurements. These measurements revealed that the maximum ridge height was 12.6 m and that the formation was grounded in 17-18 m of water. The salinity, temperature, brine volume and density of the ice were determined on samples obtained by coring. The physical characteristics of the formations as observed in satellite, SLAR and aerial imagery indicate that these formations have not moved between the time of their formation in the fall of 1974 and August of 1976. Evidence of significant aeolian debris discoloring the ice is discussed.
    Type of Medium: Series available for loan
    Pages: iv, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 76-32
    Language: English
    Note: Contents Abstract Preface Introduction Background Fast ice study area Results and discussion Literature cited
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  • 13
    Call number: ZSP-201-76/31
    In: CRREL Report, 76-31
    Description / Table of Contents: Sections in the Connecticut River where ice jam potential is high were identified through the use of low-altitude black and white photographs taken during low-flow, ice-free conditions. The hydraulics and mechanics of ice jam initiation were investigated in the river reach where these sections were identified. Certain areas were found in the river that had a high susceptibility to ice clogging, but this high potential decreased with increasing discharge because of the improved surface conveyance of the ice through the reach. The stability of ice floes was established along the channel, but the floes generally became unstable as the flow increased. This was calculated by using a Froude number criterion. Grounding locations for ice became evident when the critical Froude number was zero for a given thickness and water depth. No single factor was determined to be responsible for initiating the ice jams in the Connecticut River at Windsor. Apparently there existed a multitude of interacting conditions: surface constrictions, possible high backwater conditions from the Brattleboro Dam, a solid ice cover in the backwater of the Brattleboro Dam that prevented ice transport from the Windsor area, deep pools followed by shallow depth sections upstream of bridge piers, a greater ice thickness accumulation of fragmented floes than would result if a uniform cover could be established in the same reach, and the diurnal fluctuation of river stage casued by the release of water at Wilder Dam.
    Type of Medium: Series available for loan
    Pages: vi, 39 Seiten , Illustrationen
    Series Statement: CRREL Report 76-31
    Language: English
    Note: CONTENTS Abstract Preface Summary Conversion factors: U.S. customary to metric units of measurement Introduction Testsite Aerial photography Channel morphology — Interpretation of aerial photographs Ground surveys Hydraulic analysis Analysis of ice jam locations Winter field observations Conclusions Literature cited Appendix: Locations and plots of cross sections from Sumner Falls to Chase Island, Connecticut River
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  • 14
    Call number: MOP 44808 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 152 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 15
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/41
    In: CRREL Report, 76-41
    Description / Table of Contents: Eight Geoceiver stations were established and suitably marked along or near the crestiline of the Greenland ice sheet during GISP field operations from 1971 to 1975. At one of these stations, DYE-3, repeated Geoceiver positions indicate an ice velocity of 12.7 m.yr on an azimuth of approximately 60 degrees. Data from the International Greenland Glaciological Expedition (EGIG) surveys show that ice flow in the vicinity of Crete is radiating outward from a dome to the south. Two independent calculations of the state of equilibrium at Crete indicate ice sheet thinning rates of 0.25 to 0.37 m/yr, while direct measurement of elevation change by EGIG indicates an ice sheet thickening rate of difference of 0.06 m/yr. Resolution of these differences must await further geophysical work and deep drilling in the ice sheet.
    Type of Medium: Series available for loan
    Pages: iii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 76-41
    Language: English
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  • 16
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/43
    In: CRREL Report, 76-43
    Description / Table of Contents: Ice fog generated at the Eielson AFB power plant cooling pond contributes heavily to the total ice fog problem on the base. Several methods for ice fog suppression were studied and two techniques were tested experimentally. Experiments were also conducted to determine the magnitude of the various modes of heat transfer within the pond's microclimate. Values of evaporative and radiative heat loss during ice fog are presented. Ice cover is shown to be an effective ice fog suppression technique. Monomolecular films are also shown to be effective and offer some unique advantages, such as ease of application and low overall cost. The heat normally lost to evaporation must be dissipated by other means during suppression. With the ice cover technique this is accomplished by melting the ice cover. During suppression with monomolecular films, the heat must be dissipated by increasing radiative and convective losses. The simplicity of application of monomolecular films, along with their lower cost, combine to make this technique attractive; however, the lower pond temperatures and increased suppression effectiveness weigh heavily in favor of the ice-cover technique.
    Type of Medium: Series available for loan
    Pages: viii, 86 Seiten , Illustrationen
    Series Statement: CRREL Report 76-43
    Language: English
    Note: CONTENTS Abstract Preface List of symbols Conversion factors: U.S. customary to metric units of measurement Introduction Section I. Ice fog Section II. Evaporation Bowen's equation Evaporation equation Evaporation measurements during ice fog conditions Evaporation measurements at Eielson Power Plant cooling pond Data analysis Section Ill. Radiation during ice fog Brunt's equation Ångström equation Elsasser's equation Cloud cover Reflection Field experimental results Analysis of experimental results Radiation equations for ice fog Transmissivity of ice fog Radiation model Wind effect Summary Section IV. Convection Convective heat transfer theory Rotem and Claassen equation Kay's approach Russian approach Analysis Heat budget at the surface Conclusions Section V. Ice fog suppression techniques Fans Injection wells Latent heat storage Monomolecular films Use of heated water from the cooling pond Section VI. Latent heat storage experiments Freezing rates Cooling pond Ice building Ice growth rate -maximum system limitation Evaporation heat loss -maximum Realistic growth rate Ice building techniques Ice volume measurements Melting experiments Ice fog suppression considerations Experimental results Section VII. Recommendations and conclusions Hexadecanol studies Injection well suppression Latent heat storage suppression Comparison of approaches Measurements of evaporation Measurements of radiation loss Convective heat losses Ice fog suppression Selected bibliography Appendix A. Convective heat transfer coefficient from water to ice and from ice to air
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  • 17
    Call number: AWI A3-20-93434
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 1
    Type of Medium: Series available for loan
    Pages: 121 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,1
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 18
    Call number: MOP 45557 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 221 Seiten , Illustrationen , 21 cm
    Language: Russian
    Note: In kyrillischer Schrift
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  • 19
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/34
    In: CRREL Report, 76-34
    Description / Table of Contents: Some physical characteristics of two grounded floebergs (fragments of multi-year pressure ridges) near Prudhoe Bay, Alaska, are described. Cross-sectional profiles of the sails and keels of both floebergs were obtained. A sail to keel ratio of 1 to 3.38 obtained with one floeberg was found to be in good agreement with previous investigations. A survey of the sea floor for evidence of scoring induced during grounding yielded a maximum depth of gouging of 1.1m. Additional studies included investigations of the internal structure of the floebergs, and a brief examination of the organic and sedimentary debris found entrained within the floebergs. The grounding of ice on the continental shelves of the Arctic is of considerable interest to those concerned with the development and impact of development of these continental shelves. The field study reported here provides information useful in assessing the nature and characteristics of interactions between floebergs and the sea bed on which they are grounded.
    Type of Medium: Series available for loan
    Pages: iii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 76-34
    Language: English
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  • 20
    Call number: ZSP-201-76/35
    In: CRREL Report, 76-35
    Description / Table of Contents: Crystalline textures and fabrics of ice cores from the 2164-m-thick ice sheet at Byrd Station, Antarctica, reveal the existence of an anisotropic ice sheet. A gradual but persistent increase in the c-axis preferred orientation of the ice crystals was observed between the surface and 1200m. This progressive growth of an oriented crystal fabric is accompanied by a 20-fold increase in crystal sized between 56 and 600m, followed by virtually no change in crystal size between 6000 and 1200m. A broad vertical clustering of c-axes develops by 1200m. Between 1200 and 1300 m the structure transforms into a fine-grained mosaic of crystals with their basal glide planes now oriented substantially within the horizontal. This highly oriented fine-grained structure, which persists to 1800m, is compatible only with a strong horizontal shear deformation in this part of the ice sheet. Rapid transformation from single- to multiple-maximum fabrics occurs below 1800m. This transformation, accompanied by the growth of very large crystals, is attributed to the overriding effect of relatively high temperatures in the bottom layers of old ice at Byrd Station rather than to a significant decrease in stress. The zone of single-maximum fabrics between 1200 and 1800 m also contains numerous layers of volcanic dust. Fabrics of the very fine-grained ice associated with these dust bands indicate the bands are actively associated with shearing in the ice sheet. Some slipping of ice along the bedrock seems likely at Byrd Station, since the basal ice is at the pressure melting point and liquid water is known to exist at the ice/rock interface.
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    Pages: v, 30 Seiten , Illustrationen
    Series Statement: CRREL Report 76-35
    Language: English
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  • 21
    Call number: MOP 44439 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 68 Seiten
    Language: English
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  • 22
    Monograph available for loan
    Monograph available for loan
    [Erscheinungsort nicht ermittelbar] : [Verlag nicht ermittelbar]
    Call number: MOP 44941 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 24 Seiten
    Language: English
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  • 23
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/29
    In: CRREL Report, 79-29
    Description / Table of Contents: An analytical study of the propagation of shock waves in snow was carried out to evaluate the response of medium density snow to high rates of loading. One solution was developed for steady shock waves; this resulted in calculation of pressure jump, density jump and stress wave speed. Correlation with available experimental data was found to be good. Nonsteady shock waves were also considered in order to evaluate wave attenuation rates in snow. Very few data were available to compare with the analytical results, so no definite conclusions on the part of the study could be made. The results show, however, that shock waves that produce plastic deformation attenuate at extremely high rates and that differences in pressure between two waves are quickly eliminated within a short distance. Calculations were also made to evaluate the effect of wave frequency on attenuation rates. The results show that, for plastic waves, frequency is not a predominant factor for determining attenuation rates.
    Type of Medium: Series available for loan
    Pages: v, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-29
    Language: English
    Note: CONTENTS Abstract Preface Nomenclature I. Introduction II. A constitutive law for snow and balance principles III. Compatibility laws and jump equations for stress waves IV. Steady shock waves in snow V. Comparison of steady-wave theory with experimental results VI. A numerical solution to the nonsteady wave problem VII. Jump equations for nonsteady shock waves VIII. Reduced jump equations Discussion and conclusions Literature cited
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  • 24
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/28
    In: CRREL Report, 79-28
    Description / Table of Contents: Transmission and scanning electron micrographs of Umiat bentonite revealed thin, mica-like grains with irregular shapes. Most of the bentonite showed electron diffraction ring patterns, but some showed hexagonal net patterns as well as ring patterns. The lengths of the unit cells were calculated to be 5.18 A along the a-axis and 8.97 A along the b-axis. Semiquantitative analyses were made using an energy dispersive spectrometer. Common elements such as Si, Ti, Al, Fe, Mg, Na and K were determined. The molecular ratio of SiO2:Al2O3 was calculated to be 492:100 for the bulk sample, indicating that Umiat bentonite is similar in most respects to Wyoming bentonite, and is classified as a mont-morillonite. The microstructure of frozen Umiat bentonite was observed at a specimen temperature of -100 C using a scanning electron microscope equipped with a cold stage. Frozen bentonite and segregated ice patterns formed from wet bentonite were examined using an X-ray map and Si X-ray line scan. Sublimation processes of ice in the frozen bentonite were observed at specimen temperatures of -60 and -80 C. After sublimation of the ice the bentonite displayed a honeycomb structure. It was concluded that the freezing-sublimation cycle in frozen soil increases the permeability of water vapor due to the three-dimensional structure of the coagulated clay formed by freezing.
    Type of Medium: Series available for loan
    Pages: iii, 14 Seiten , Illustrationen
    Series Statement: CRREL Report 79-28
    Language: English
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  • 25
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/25
    In: CRREL Report, 79-25
    In: Charged dislocation in ice, I.
    Description / Table of Contents: The motion of dislocations in single crystal ice under an electric field was observed by using X-ray topographic methods. Electric charge density on these dislocations was deduced from the amplitude and length of the dislocation segment under the known AC electrical field. The most likely linear charge density was about +5x10^-11 c/m, although considerable variation is possible depending on the effective field acting on the dislocation lines.
    Type of Medium: Series available for loan
    Pages: iii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-25
    Language: English
    Note: CONTENTS Abstract Preface Introduction Theory Experimental apparatus and procedure Results Discussion Concluding remarks Selected bibliography Appendix A. Mosotti type field on core of cylindrical cavity
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  • 26
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/24
    In: CRREL Report, 79-24
    Description / Table of Contents: By using a new thermocoring technique, a hole was successfully drilled through the 416-m thickness of the Ross Ice Shelf at J-9 Camp. This report provides a description of the drill and an account of this drilling project. A provisional examination of the core shows the ice shelf to consist of 410 m of snow and glacial ice underlain by 6 m of sea ice formed by direct freezing of sea water to the bottom of the Ross Ice Shelf.
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    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-24
    Language: English
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  • 27
    Call number: ZSP-201-79/23
    In: CRREL Report, 79-23
    Description / Table of Contents: The performance of surface impedance and magnetic induction electromagnetic subsurface exploration techniques was studied seasonally at various sites in Alaska where permafrost and massive ground ice occurred. The surface impedance method, which uses radiowaves in the LF and VLF bands, and the magnetic induction method, which uses low-frequency magnetic induction fields, distinguish subsurface materials by the electrical resistivity of the materials. The methods used have greatest sensitivity within about 20 m of the surface and are, therefore, most applicable for shallow subsurface investigations. The selection of study sites was based on anticipated contrasts in electrical resistivity between ground ice and adjacent earth materials. A magnetic induction instrument, using a separation of 3.66-m between the transmitter and receiver antennas, in general was able to detect near-surface zones of massive ice and to provide data regarding permafrost distribution in both the Fairbanks and Prudhoe Bay areas. At this antenna separation, the depth of magnetic field penetration was sufficient to include mainly the zone containing maximum contrasts in resistivity between ground ice and other earth materials. In the Fairbanks area, contrasts, in this zone were greatest in late winter when the seasonally thawed surface layer was completely frozen. When thawed, this layer usually becomes more conductive and often masks the deeper resistivity contrasts. In the Prudhoe Bay area, maximum ground resistivity contrasts were detected in late summer when shallow subsurface temperatures had risen sufficiently to permit resistivity contrasts between the massive ice and the ice-rich ground to appear.
    Type of Medium: Series available for loan
    Pages: v, 24 Seiten , Illustrationen
    Series Statement: CRREL Report 79-23
    Language: English
    Note: CONTENTS Abstract Preface Introduction Background Obiectives and procedures Ground electrical resistivity in permafrost regions Electromagnetic techniques General Magnetic induction method Surface impedance fradiowave method Direct current method General description of field sites Results Site 1 CRREL permafrost station, Fairbanks, Alaska Site 2 Planned road cut for Steese Highway near Fox, Alaska Site 3 Relic floodplain near Fairbanks, Alaska Site 4 Pingos, Prudhoe Bay, Alaska Site 5 Ice wedges, Prudhoe Bay, Alaska Comparisons between the surface impedance and magnetic induction methods Conclusions and recommendations Literature cited Appendix A. Discussion of the depth of sensitivity of the magnetic induction method using two- and three-layer apparent resistivity curves
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  • 28
    Call number: MOP 47630 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 240 Seiten , Illustrationen
    Edition: 7., bearbeitete und erweiterte Auflage
    Language: German
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  • 29
    Journal available for loan
    Journal available for loan
    Republique Tunisienne : Ministere du Transport
    Call number: MOP 47385 / Mitte
    Type of Medium: Journal available for loan
    Pages: circa 200 Seiten
    Series Statement: Almanach / Institut National de la Meteorologie 1991
    Language: French
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  • 30
    Call number: MOP 46654 / Mitte
    In: World weather program : plan for fiscal year, 1980 and 1981
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  • 31
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/27
    In: CRREL Report, 79-27
    Description / Table of Contents: Some Bessel function identities found by solving problems of the deflection of a floating ice plate by two different methods are rigorously proved. The master formulas from which all the identities are derived are in a Fourier reciprocal relationship, connecting a Hankel function to an exponential function. Many new formulas can be derived from the master formulas. The analytical method presented here now opens the way to study a hitherto impossible type of problem--the deflection of floating elastic plates of various shapes and boundary conditions.
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    Pages: ii, 13 Seiten , Illustrationen
    Series Statement: CRREL Report 79-27
    Language: English
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  • 32
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/26
    In: CRREL Report, 79-26
    Description / Table of Contents: A 19-year record of the annual closing and opening dates of operation of the Lake Champlain ferry at Grand Isle, Vermont, which are controlled by the lake's ice cover, was made available to CRREL. These navigation records accurately approximated the freeze-over and breakup dates for the ferry crossing area between Gordon Landing, Vermont, and Cumberland Head, New York. When compared statistically with water temperature and climatological data for the same years at nearby Lake Champlain locations, the dates allowed accurate predictions of ice formation. From nearby air temperature records, cumulative freezing degree-day (deg C) curves were plotted for each year of record, and ice formation dates and standard deviations were predicted with considerable accuracy. Several methods of predicting ice formation on Lake Champlain were attempted. The most accurate approach used a combination of water temperatures and freezing degree-days. The influence of wind speed on ice cover formation and prediction are also discussed in the report.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-26
    Language: English
    Note: CONTENTS Abstract Preface Introduction Data tabulation and collection Air temperatures 11-reezing degree-days Water temperatures Closing and opening dates Results Air temperature Freezing degree-days Water temperatures Analysis: Attempted methods of predicting ice formation Predicting air temperatures 8Summer water temperatures Fall water temperatures and freezing degree-days Wind speed influence on closing of the lake Water temperature vs surface air temperature analysis Prediction of ice-out dates Conclusions Literature cited Appendix A. Freezing degree-day curves with ice notations and watertemperature notations Appendix B. Summary
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  • 33
    Monograph available for loan
    Monograph available for loan
    Leipzig : Akademische Verlagsgesellschaft Geest u. Portig
    Associated volumes
    Call number: 11539
    In: Technisch-physikalische Monographien
    Type of Medium: Monograph available for loan
    Pages: 467 Seiten , Illustrationen , 22 cm
    Edition: 1. Aufl
    Series Statement: Technisch-physikalische Monographien 37
    Language: Undetermined
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  • 34
    Call number: AWI Bio-20-94333
    Type of Medium: Monograph available for loan
    Pages: 493 Seiten , Illustrationen
    Edition: 1. Auflage
    ISBN: 3437302264 , 9783437302268
    Series Statement: Algenflora der Ostsee / Helmut Pankow 2
    Language: German
    Note: Inhaltsverzeichnis Vorwort Übersicht über das verwendete Halobiensystem Gruppenschlüssel Cyanophyta Cyanophyceae Chroococcales Chroococcaceae 1. Microcystis 2. Aphanothece 3. Chroococcus 4. Gloeothece 5. Gomphosphaeria 6. Coelosphaerium 7. Merismopedia 8. Microcrocis 9. Dactylococcopsis Nostocales Rivulariaceae 1. Gloeotrichia Scytonemataceae 1. Tolypothrix N ostocaceae 1. Nostoc 2. Aphanizomenon 3. Nodularia 4. Anabaena Pelonemataceae 1. Achroonema Oscillatoriaceae 1. Spirulina 2. Oscillatoria 3. Lyngbya Chrysophyta Chrysophyceae Chrysomonadales Chrysomonadineae Dino bryonaceae 1. Dinobryon Prymnesiaceae 1. Prymnesium Synuraceae 1. Synura 2. Microglena Chrysococcaceae 1. Chrysococcus 2. Bicoeca Ochromonadaceae 1. Ochromonas 2. Uroglena Coccolithineae Coccolithaceae 1. Gephyrocapsa 2. Discosphaera Dictyochineae (= Silicoflagellatae) Dictyochaceae 1. Dictyocha Chrysocapsales Phaeocystaceae 1. Phaeocystis Ebriales Ebriaceae 1. Ebria Xanthophyceae (= Heterokontae) Rhizochloridales Rhizochloridaceae 1. Rhizochloris Mischococcales ( = Heterococcales) Pleurochloridaceae 1. Meringosphaera Halosphaeraceae 1. Halosphaera Craspedophyceae (= farblose Flagellaten unsicherer Stellung) Craspedomonadophycideae (= Choanoflagellatae) Monosigales Monosigaceae Inhaltsverzeichnis 1. Proterospongia Diatomaphyceae Centrophycideae Coscinodiscales Coscinodiscaceae 1. Melosira 2. Paralia 3. Hyalodiscus 4. Podosira 5. Stephanopyxis 6. Sceletonema 7. Coscinosira 8. Thalassiosira 9. Cyclotella 10. Stephanodiscus 11. Coscinodiscus Actinodiscaceae 1. Actinoptychus Eupodiscaceae 1. Actinocyclus 2. Auliscus Rhizosoleniales Rhizosoleniaceae 1. Rhizosolenia 2. Guinardia 3. Lithodesmium 4. Ditylum 5. Detonula 6. Lauderia 7. Leptocylindrus Biddulphiales Chaetoceraceae 1. Chaetoceros Biddulphiaceae 1. Cerataulus 2. Attheya 3. Biddulphia Hemiaulaceae 1. Cerataulina Anaulaceae 1. Anaulus Pennatophycideae Diatomales Diatomaceae 1. Licmophora 2. Grammatophora 3. Tabellaria 4. Rhabdonema 5. Striatella 6. Hustedtiella 7. Plagiogramma 8. Diatoma 9. Thalassionema 10. Asterionella 11. Opephora 12. Synedra 13. Glyphodesmis 14. Cymatosira 15. Dimerogramma 16. Raphoneis 17. Fragilaria 18. Catenula Auriculaceae 1. Auricula Aehnanthales Achnanthaceae 1. Cocconeis 2. Achnanthes 3. Rhoicosphenia Naviculales Naviculaceae 1. Amphiprora 2. Tropidoneis 3. Mastogloia 4. Gyrosigma 5. Pleurosigma 6. Scoliotropis 7. Scoliopleura 8. Diploneis 9. Stenoneis 10. Amphipleura 11. Frustulia 12. Pinnularia 13. Trachyneis 14. Caloneis 15. Pseudoamphiprora 16. Stauroneis 17. Brebissonia 18. Anomoeoneis 19. Navicula 20. Gomphonema 21. Cymbella 22. Amphora Epithemiaceae 1. Epithemia 2. Rhopalodia Nitzschiaceae 1. Cylindrotheca 2. Bacillaria 3. Hantzschia 4. Nitzschia Surirellaceae 1. Cymatopleura 2. Surirella 3. Campylodiscus Pyrrhophyta Cryptophyceae Cryptomonadales Cryptomonadaceae 1. Chroomonas 2. Cryptomonas Desmophyceae Prorocentrales Prorocentraceae 1. Exuviella 2. Prorocentrum Dinophysiales Dinophysidaceae l, Dinophysis Dinophyceae Peridiniales Gymnodiniaceae 1. Gymnodinium 2. Amphidinium 3. Katodinium 4. Cochlodinium 5. Gyrodinium Polykrikaceae 1. Polykrikos Warnowiaceae 1. Warnowia N octilucaceae 1. Noctiluca Glenodiniaceae 1. Diplopeltopsis 2. Glenodinium Glenodiniopsidaceae 1. Hemidinium 2. Pyrophacus Pronoctilucaceae 1. Pronoctiluca Peridiniaceae 1. Minuscula 2. Peridinium 3. Heterocapsa Gonyaulacaceae 1. Gonyaulax 2. Amphidiniopsis Protoceratiaceae 1. Protoceratium Ceratiaceae 1. Ceratium Goniodomaceae 1. Goniodoma Cladopyxiaceae 1. Cladopyxis Dinococcales Dinococcaceae 1. Dissodinium Chlorophyta Chlorophyceae Pyramimonadales Pyramimonadaceae Volvocales Chlamydomonadaceae 1. Chlamydomonas 2. Carteria 3. Pachysphaera Volvocaceae 1. Gonium 2. Pandorina 3. Eudorina 4. Volvox Chlorococcales Hydrodictyaceae 1. Pediastrum Micractiniaceae 1. Golenkinia 2. Micractinium Dictyosphaeraceae 1. Dictyosphaerium 2. Botryococcus Oocystaceae 1. Chodatella 2. Lagerheimia 3. Franceia 4. Oocystis 5. Tetraedron 6. Monoraphidium 7. Ankistrodesmus 8. Schroederia Scenedesmaceae 1. Scenedesmus 2. Crucigenia 3. Tetrastrum 4. Actinastrum 5. Coelastrum Ulotrichales Ulotrichaceae 1. Binuclearia Conjugatophyceae Desmidiales Desmidiaceae 1. Cosmarium 2. Closterium 3. Staurastrum Euglenophyta Euglenophyceae Euglenales Euglenaceae 1. Colacium 2. Euglena 3. Lepocinclis 4. Phacus Eutreptiaceae 1. Eutreptia Literatur Literaturnachtrag zu Band I Tafelanhang Nachtrag zu Band I Index
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  • 35
    Call number: AWI G3-22-94980
    In: Bochumer geographische Arbeiten, 35
    Type of Medium: Series available for loan
    Pages: XI, 211 Seiten , Illustrationen
    ISBN: 3-506-71215-2
    Series Statement: Bochumer geographische Arbeiten 35
    Language: German
    Note: Zugleich: Dissertation, Ruhr-Universität Bochum, 1978 , lnhal tsverzeichnis Verzeichnis der Abbildungen Verzeichnis der tabellarischen Übersichten 1. Einleitung 1.1 Terminologische Fragen 2. Die bisherige Diskussion um die Definition des Periglaziarbegriffes 3. Einführung in die Problematik und Schwerpunkte dieser Untersuchung 3.1 Unterschiedliche Definitionsansätze 3.2 Das Problem aus geographischer Sicht 3.3 Das Problem aus palaoqeographisch-geologischer Sicht 3.4 Schwerpunkte und Arbeitsweise der weiteren Untersuchung 4. Die Einflußnahme periglaziärer Milieufaktoren im Überblick 4.1 Direkt- und indirekt-klimatische Steuerungsfaktoren 4.2 Aklimatische Steuerunqsfaktoren 5. Klimatische und geographische Bodenqefrornistypen 5.1 Dauerfrostboden mit jahreszeitlicher Auftauschicht 5.1.1 Terminologische Fragen und die räumliche Gliederung des Dauerfrostbodens 5.1.2 Die thermische Vertikalqliederung des oberflächennahen Dauerfrostbodens 5.1.3 Zur Verbreitung und klimatischen Abgrenzung des Dauerfrostbodens 5.2 Jahreszeitliche Bodengefrornis 5.3 Tageszeitliche und kurzperiodische Bodengefrornis 5.4 Kammeis 6. Analyse der Bildung, Verbreitung und Differenzierunq wichtiger rezenter Periglaziarerscheinungen und Bewertung ihrer Verwendbarkeit als Definitionskriterien des Periglaziärs 6.1 Periglaziäre Prozesse und periglaziäre Formen im engeren Sinne (Periglaziäre Mikroformung) 6.1.1 Formen der Bodenmusterung ohne Detritussortierung (Texturböden) 6.1.1.1 Kongelikontraktionsformen mit Spalteneis (Eiskeilpolygone) 6.1.1.2 Kongelikontraktionsformen ohne Spalteneis (Sandkeilpolygone) 6.1.1.3 Frostspaltenmakropolygone und Mollisolfrostkeile 6.1.1.4 Spaltenmikropolygone ('Zellenböden') 6.1.1.5 Erdbülten (Thufur) 6.1.1.6 Nichtsortierte Feinerdekreise (Mudpits) 6.1. 2 Frost- und Eishügelformen 6.1.2.1 Saisonale Frosthügel 6.1.2.2 Palsas 6.1.2.3 Pingos und pingoähnliche Formen 6.1.3 Strangmoore 6.1.4 Formen der Bodenmusterung mit Detritussortierung (Strukturböden) 6.1.5 Periglaziär-denudative Prozesse und Formen im engeren Sinne - Kleinformen der Gelisolifluktion 6.1. 5.1 Erscheinungen der amorphen Gelisolifluktion 6.1.5.2 Kleinformen der differenzierten Gelisolifluktion 6.1.5.3 Zusammenfassung und Ergebnisse 6.1.6 Blockgletscher 6.1.7 Vorgänge und Formen der Nivation und Kryoplanation 6.1.8 Dauerfrostboden-Degradation und Depergelationsformen 6.1.8.1 Depergelationsformen infolge vertikaler Dauerfrostboden-Degradation 6.1.8.2 Depergelationsformen infolge lateraler Dauerfrostboden-Degradation 6.2 Periglaziäre Prozesse und Formen im weiteren Sinne (Periglaziäre Meso- und Makroformung) 6.3 Zusammenfassung der klimageomorphologischen Leitformenwerte 7. Zur räumlichen Abgrenzung und regionalen Differenzierung der periglaziären Zone und Höhenstufe - planetarischer und hypsometrischer Wandel der periglaziären Formung 7.1 Grundlagen und Kriterienl der räumlichen Abgrenzung des Periglaziärs 7.2 Kriterien der regionalen Differenzierung des Periglaziärs 7.3 Die Abgrenzung und regionale Differenzierung der periglaziären Zone 7.3.1 Subpolar-ozeanisches Periglaziär 7.3.1.1 Subpolar-hochozeanisches Periglaziär 7.3.2 Subpolar-kontinentales Periqlaziär (subpolares Subperiglaziär) 7.3.3 Polares Periglaziär 7.3.3.1 Polares Tundrenperiglaziär 7.3.3.2 Polares Frostschuttperiglaziär 7.3.4 Hochpolares Frostschuttperiglaziär und antarktisches Periglaziär 7.3.5 Hochkontinentales Boreal-Periglaziär 7.3.6 Zusammenfassung und Ergebnisse 7.4 Abgrenzung, Untergrenzverlauf und hypsometrische Differenzierung der periglaziären Höherstufe 7.4.1 Subpolar-periglaziäre Höhenstufe 7.4.2 Mediolatitudinal-periglaziäre Höhenstufe 7.4.3 Zur Frage einer periglaziären Höhenstufe in den Sub- und Randtropen 7.4.4 Tropisch-periglaziäre Höhenstufe 7.4.5 Zusammenfassung 8. Zusammenfassung und Ergebnisse Summary Literaturverzeichnis , Zusammenfassung in deutscher und englischer Sprache
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  • 36
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/29
    In: CRREL Report, 76-29
    Description / Table of Contents: In order to verify current theoretical equations on ice bearing capacity, a heavily loaded truck was used to make successive passes over two ice bridges. Equipment, weather and the normal problems associated with field work resulted in only one complete breakthrough test. Breakthrough occurred on one bridge with a vehicle weight of 53,630 lb (24,327 kg) and an ice thickness of 17.5 in. (44.5 cm). Since only one test was completed, the conclusions drawn cannot be unequivocal. However, the results do indicate that Nevel's equation for ultimate failure of a floating ice sheet is a good working tool.
    Type of Medium: Series available for loan
    Pages: iv, 19 Seiten , Illustrationen
    Series Statement: CRREL Report 76-29
    Language: English
    Note: Contents Abstract Preface Summary Introduction Location Test procedure Loading Site preparation and bridge construction Deflection measurements Conclusions Literature cited Appendix, Test data
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  • 37
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/44
    In: CRREL Report, 76-44
    Description / Table of Contents: The deformation of wet snow is explained in terms of the thermodynamics of the three phases of water. When deformation by particle rearrangement is fully developed, deformation can occur most rapidly by melting at the particle contacts. The rate of deformation is highly sensitive to the liquid water content, ionic impurity content, particle contact area, and stress level. A model of the hydrostatic deformation of wet snow is constructed, and examples of the deformation of wet snow are given for a variety of conditions. These results are in agreement with existing experimental evidence. The model accurately simulates the transient nature of the deformation and the effect of water content on the quasi-stable density of wet snow subjected to a constant stress.
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    Pages: iv, 9 Seiten , Illustrationen
    Series Statement: CRREL Report 76-44
    Language: English
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  • 38
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
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    Call number: ZSP-201-76/47
    In: CRREL Report, 76-47
    Description / Table of Contents: This report describes two mechanical ice-cutting systems for the removal of ice collars at the high pool level on the Poe Lock of the St. Marys Falls Canal at Sault Ste. Marie, Michigan. One system was a narrow-kerf (3.25-in.-wide) coal-cutting chain saw mounted on a bar, driven by a 65-hp wheeled trencher. The other system was a lumber-cutting chain saw mounted on a bar, driven by a 30-hp wheeled soil trencher which cut a 0.56-in.-wide kerf. The lumber-cutting saw's bar was too flexible and the desired cutting traverse speed was not met. The coal-cutting saw cut 6-ft-deep ice collars at traverse speeds of up to 10 ft/min and is acceptable. With a few modifications, the coal-cutting saw would be operational.
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    Pages: iii, 20 Seiten , Illustrationen
    Series Statement: CRREL Report 76-47
    Language: English
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  • 39
    Call number: MOP 44818 / Mitte
    Type of Medium: Monograph available for loan
    Pages: vii, 50 Seiten , 28 cm
    Language: English
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  • 40
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/9
    In: CRREL Report, 79-9
    Description / Table of Contents: Sedimentation at the terminus of the Matanuska Glacier has been found to be primarily subaerial in a 100- to 300-m wide, ice-cored zone paralleling the edge of the active ice. Certain physical and chemical characteristics of the ice and debris of the superglacial, englacial and basal zones of the glacier indicate the debris of the basal zone, the primary source of sediment, is entrained during freeze-on of meltwater, probably surficially derived, to the glacier sole. Till formation results from the melting of buried ice of the basal zone. Melt-out till inherits the texture and particle orientations of basal ice debris; other properties are not as well preserved. Most deposits result from resedimentation of till and debris by sediment gravity flows, meltwater sheet and rill flow, slump, spall, and ice ablation. Depositional processes are interrelated in the process of backwasting of ice-cored slopes. Sediment flows are the primary process of resedimentation. Their physical characteristics, multiple mechanisms of flow and deposition, and characteristics of their deposits vary with the water content of the flow mass. Deposits of each process are distinguished from one another by detailed analysis of their internal organization, geometry and dimensions, and the presence of other internal and related external features. Genetic facies are defined by these characteristics. The interrelationship of processes develops a composite depositional sequence defined in terms of genetic facies associations; an upper, resedimented facies association, a middile, till facies association, and a lower, subglacial-resedimental facies association. The lateral and vertical distribution of genetic facies within the associations is mainly nonrepetitive.
    Type of Medium: Series available for loan
    Pages: X, 112 Seiten , Illustrationen , 1 Beilage
    Series Statement: CRREL Report 79-9
    Language: English
    Note: CONTENTS Abstract Preface Summary Chapter 1. Introduction Field site Historical background Chapter 2. Characteristics of the debris and ice Characteristics of the facies and subfacies Basal zone Characteristics of the debris Discussion Chapter 3. Oxygen isotope analysis Sampling and analysis Results Discussion Chapter 4. Depositional processes—till formation Methods of analysis Environmental setting Till formation Chapter 5. Depositional processes—resedimentation Sediment flows Other resedimentation processes Resedimentation process relationships Chapter 6. Process distribution, sediment dispersal and depositional patterns Physical characteristics Sediment dispersal Sedimentary facies Patterns of terminus sedimentation Chapter 7. Conclusions Literature cited
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  • 41
    Call number: MOP 45476 / Mitte
    Type of Medium: Monograph available for loan
    Pages: [400] Seiten , Illustrationen , 28 cm
    Language: English
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  • 42
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    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/21
    In: CRREL Report, 79-21
    Description / Table of Contents: The report studies the question of whether Great Lakes freighters could move effectively through ice-clogged channels with the aid of tows provided by warping or kedging systems. Ten operational concepts are outlined, and their advantages and disadvantages are noted. The crushing resistance of floating brash ice is then analyzed. The neutral, active and passive states of stress for laterally confined brash ice are considered, and the resistance to horizontal thrusting by a smooth vertical wall is calculated for cohesionless brash ice, and for ice in which there is finite cohesion between the ice fragments. The thickening of the ice cover in the vicinity of a "pusher", and the formation of pressure ridges, are analyzed in order to estimate the amount of pile-up that can occur against a ship hull. The analysis then moves on to consideration of ship resistance by brash ice, taking into account crushing resistance at the bow, tangential friction at the bow, and hull friction aft of the bow section. Comparisons are made between thrust from the ship’s screws and the calculated ice resistance. The next section of the report estimates the force requirements for a warping or kedging system in terms of thrust augmentation for existing vessels. Tow cable requirements are given, and estimates are made for cable anchors and for anchorage of underwater structures. The force and power requirements for winches and windlasses are given, the practical problems involved in the pickup or transfer of cables are mentioned, and the report concludes with a brief appraisal. The conclusion is that a simple warping tug system is appropriate for a full scale experiment, a chain ferry with auxiliary barge seems attractive for an operational system, and a chain ferry plow may be an efficient way to clear ice from channels.
    Type of Medium: Series available for loan
    Pages: iv, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-21
    Language: English
    Note: CONTENTS Abstract Preface Introduction Operational concepts A. Warping tug system B. Chain ferry system C. Chain ferry with auxiliary barge D. Ski tow system E. Dual winch warping system F. Simple kedging G. Trailing-line system H. Above-surface dual winch system I. Pulley systems J. Chain ferry plow Crushing resistance of fragmented ice covers Resistance to ship passage by broken ice Crushing resistance at the bow Tangential friction at the bow Hull friction aft of the bow section Total ship resistance from brash ice Comparison of ship thrust and ice resistance Force requirements for a warping or kedging system Tow cable requirements Anchors and anchorages Force and power requirements for winches and windlasses Pickup or transfer of cable General appraisal Literature cited
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  • 43
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    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-76/26
    In: CRREL Report, 76-26
    Description / Table of Contents: Debris over a 44-mile stretch of the Chena River was studied. The study area extended from the first bridge on the Chena Hot Springs Road to the Chena River Flood Control damsite. The purpose of the study was to assess the potential danger to the Chena River Flood Control Dam outlet structure. Debris was catalogued, log jams were measured, and sources of debris were studied. The average size of logs was determined, as well as the number of logs present on the river. The authors concluded that a serious debris problem existed and would remain serious for the foreseeable future. Recommendations for debris handling were made.
    Type of Medium: Series available for loan
    Pages: iv, 17 Seiten , Illustrationen
    Series Statement: CRREL Report 76-26
    Language: English
    Note: Contents Abstract Preface Summary Introduction Origin of debris Volume, magnitude Types of debris Hazards of the debris Recommended measures to counteract log jamming Conclusions and recommendations Future work Epilogue Selected bibliography Appendix: Additional photographs of Chena River debris
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  • 44
    Call number: MOP 40847 / Mitte
    Type of Medium: Monograph available for loan
    Pages: x, 424 Seiten
    Language: English
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  • 45
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 40419 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 302 Seiten , Illustrationen
    Language: Russian
    Note: Zsfassung in englischer Sprache , In kyrillischer Schrift
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  • 46
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Call number: MOP 45690 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 263 Seiten , Illustrationen
    Language: Russian
    Note: In kyrillischer Schrift
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  • 47
    Journal available for loan
    Journal available for loan
    Republique Tunisienne : Ministere du Transport
    Call number: MOP 47385 / Mitte
    Type of Medium: Journal available for loan
    Pages: circa 200 Seiten
    Series Statement: Almanach / Institut National de la Meteorologie 1989
    Language: French
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  • 48
    Journal available for loan
    Journal available for loan
    Republique Tunisienne : Ministere du Transport
    Call number: MOP 47385 / Mitte
    Type of Medium: Journal available for loan
    Pages: circa 200 Seiten
    Series Statement: Almanach / Institut National de la Meteorologie 1990
    Language: French
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  • 49
    Call number: AWI A3-20-93434-2
    In: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin, Band XXXII, Heft 2
    Type of Medium: Series available for loan
    Pages: 218 Seiten , Illustrationen
    Series Statement: Meteorologische Abhandlungen / Institut für Meteorologie und Geophysik der Freien Universität Berlin 32,2
    Language: German
    Note: Zugleich: Dissertation, Freie Unversität Berlin, [ca. 1963] , INHALTSVERZEICHNIS PROBLEMSTELLUNG UND ZIELSETZUNG 1. BEMERKUNGEN ZUM BEOBACHTUNGSGELÄNDE UND ZUM BEOBACHTUNGSMATERIAL 1.1 Das Beobachtungsgelände 1.2 Das Beobachtungsmaterial 2. HOMOGENITÄTSBETRACHTUNGEN 2.1 Temperatur 2.2 Niederschlag 2.3 Wind 2.4 Sonnenschein und Bewölkung 3. TEMPERATURVERHÄLTNISSE 3.1 Monats- und Jahreswerte 3.2 Tageswerte 3.3 Pentadenwerte 3.4 Häufigkeitsbetrachtungen 3.5 Interdiurne Veränderlichkeit 3.6 Der tägliche Gang 3.7 Vorkommen bestimmter Schwellenwerte 3.71 Frost- und Eistage 3.72 Sommer- und Tropentage 4. DER WASSERGEHALT DER LUFT 4.1 Monats- und Jahreswerte 4.2 Tageswerte 4.3 Häufigkeitsbetrachtungen 4.4 Interdiurne Veränderlichkeit 4.5 Der tägliche Gang 5. BEWÖLKUNGSVERHÄLTNISSE 5.1 Monats- und Jahreswerte 5.2 Tageswerte 5.3 Häufigkeitsbetrachtungen 5.4 Der tägliche Gang 5.5 Heitere und trübe Tage 5.6 Nebel 6. SONNENSCHEIN 6.1 Monats- und Jahreswerte 6.2 Tageswerte 6.3 Der tägliche Gang 7. NIEDERSCHLAGSVERHÄLTNISSE 7.1 Monats- und Jahreswerte 7.2 Niederschlagsbereitschaft 7.3 Tageswerte 7.4 Der tägliche Gang 7.5 Häufigkeitsbetrachtungen 7.6 Niederschlags- und Trockenperioden 7.7 Niederschlag und Wind· 7.8 Schneeverhältnisse 7.81 Schneefall und Schneedecke 7.82 Schneehöhe 7.9 Gewitter 8. WINDVERHÄLTNISSE 8.1 Windrichtung 8.2 Windgeschwindigkeit 8.21 Der jährliche Gang 8.22 Häufigkeitsbetrachtungen 8.23 Sturmtage und Windstillen 8.24 Der tägliche Gang 9.ZUSAMMENFASSUNG VERZEICHNIS DER TEXTTABELLEN VERZEICHNIS DER ABBILDUNGEN LITERATURVERZEICHNIS TABELLENANHANG
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  • 50
    Monograph available for loan
    Monograph available for loan
    Oak Ridge, Tenn. : U.S. Department of Energy
    Call number: MOP 44436 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 15, 3, 5 Seiten
    Language: English
    Note: The field experiments were continued to estimate convective storm particulate scavenging efficiency in proximity to the St. Louis, Missouri urban-industrial complex. Complementary studies of the urban aerosol characterization, source strength, and removal processes were also studied. The 1975 field effort shifted emphasis from the immediate St. Louis area to the Alton-Wood River industrial complex. Along with the change in size and configuration of the network, there were increases in the numbers of most types of samplers. The new network yielded the following types of samples for analysis and interpretation: 1065 total rain samples from 85 sites; 68 sequential rainwater samples from 2 locations; 272 wet/dry samples from 7 locations; 216 air filter samples from 7 locations; 36 air filter samples from aircraft; and raindrop spectrometer data from 11 sites for the period 17 June-18 August. The analysis procedures require that all water samples undergo filtering for separate analyses of soluble and insoluble fractions of the elemental concentrations. This data collection effort provided a record number of samples for chemical analysis. Approximately 4000 pibals and over 370 radiosondes were released in the operational period, providing wind and thermodynamic data on 33 days. Aircraft missions were flown on 24 days, with one air tracer release of cesium on 19 July 1975. The status of the analysis of all types of data is described.
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  • 51
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/14
    In: CRREL Report, 79-14
    Description / Table of Contents: Solid ice growth rates due to the presence of frazil slush beneath the ice cover have been shown to be greater than the so-called static growth. The frazil slush reduces the effective heat of ice solidification and the frazil particles freeze into the interstitial water. Numerical schemes are presented which clearly show the effect of frazil ice porosity on ice cover growth rates and the numerical model using air temperature as the major input is compared with field data on ice thickness in a small river laden with frazil ice beneath its cover.
    Type of Medium: Series available for loan
    Pages: ii, 4 Seiten , Illustrationen
    Series Statement: CRREL Report 79-14
    Language: English
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  • 52
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/22
    In: CRREL Report, 79-22
    Description / Table of Contents: Field observations at 60 Sites located in the fast or near-fast ice along a 1200-km stretch of the north coast of Alaska between Bering Strait and Barter Island have shown that the great majority of the ice samples (95%) exhibit striking c-axis alignments within the horizontal plane. Such alignments were usually well developed by the time the ice was 50 cm thick and in some cases when the ice was 20 cm thick. In all cases the degree of preferred orientation increased with depth in the ice. Representative standard deviations around a mean direction in the horizontal plane are commonly less than ± 10° for samples collected near the bottom of the ice. The general patterns of the alignments support a correlation between the preferred c-axis direction and the current direction at the ice/water interface. A comparison between c-axis alignments and spot current measurements made at 42 locations shows that the most frequent current direction coincides with the mean c-axis direction. Such alignments are believed to be the result of geometric selection with the most favored orientation being that in which the current flows normal to the (0001) plates of ice that compose the dendritic sea ice/sea water interface.
    Type of Medium: Series available for loan
    Pages: v, 21 Seiten , Illustrationen
    Series Statement: CRREL Report 79-22
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Techniques and sampling Observations Crystal alignments “Odd” sites Causes Conclusions Literature cited Appendix A: Current observations
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  • 53
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/19
    In: CRREL Report, 79-19
    Description / Table of Contents: The critical velocities of loads moving over floating ice plates have been determined by several authors. In all these analyses it was assumed that the in-plane force field in the ice cover is zero. However, due to constrained thermal strains, in-plane forces do occur in the field. The purpose of the present paper is to determine their effect upon the critical velocities of the moving loads. It is shown that a uniform compression force field reduces the critical velocity, whereas a tension force field has the opposite effect.
    Type of Medium: Series available for loan
    Pages: ii, 12 Seiten , Illustrationen
    Series Statement: CRREL Report 79-19
    Language: English
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  • 54
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/17
    In: CRREL Report, 79-17
    Description / Table of Contents: Six test roofs of two different slopes — 16.3° and 39.8°, and three different roof coverings — asphalt shingles, cedar shingles, and corrugated aluminum sheeting, were constructed at USACRREL, Hanover, New Hampshire, and were instrumented with thermocouples, heat flow meters, and calibrated gutters. Measurements were recorded for the winters of 1971-72 and 1972-73. The degree of icing and the chronological changes in the snow cover were recorded on 35-mm Kodachrome slides. It was found that eave icing is a sensitive function of the slope, roof covering composi­tion, and solar radiation. The effects of wind were not investigated; the data were screened to remove all informa­tion corresponding to windspeeds over 8 km/h. In order of increasing tendency to form ice dams on the eaves, the roofs were high-slope asphalt, high-slope cedar, high-slope aluminum, low-slope asphalt, low-slope cedar, and low- slope aluminum.
    Type of Medium: Series available for loan
    Pages: vi, 40 Seiten , Illustrationen
    Series Statement: CRREL Report 79-17
    Language: English
    Note: CONTENTS Abstract Preface Summary Introduction Experimental procedure Description of roofs Meteorological data Procedure Analysis General Temperature profiles Temperature rankings Heat flow Snow depths and meltwater volumes Degree of icing Results and conclusions General Temperature profiles of the roofs Comparative temperatures of roofs by section — rankings Heat flow and accumulation Snow depth, coverage, and meltwater Degree of icing Discussion of the icing problem Literature cited
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  • 55
    Series available for loan
    Series available for loan
    Hanover, NH : U.S. Army Cold Regions Research and Engineering Laboratory
    Associated volumes
    Call number: ZSP-201-79/16
    In: CRREL Report, 79-16
    Description / Table of Contents: In 1973 two membrane encapsulated soil layer (MESL) test sections were constructed into existing gravel surfaced roads at Elmendorf A FB and at Ft. Wainwright in Anchorage and Fairbanks, Alaska, respectively. The Elmendorf AFB MESL contains a silty clay soil and the Ft. Wainwright MESL contains a nonplastic silt. Both sections were constructed at soil moisture contents of approximately 2% to 3% below optimum for the CE-12 compactive effort. There were no indica­tions of soil moisture migration during freezing in either test section and after-thaw field California Bearing Ratio values were nearly equal to values measured before freezing. There is growing evidence of a slight increase in the overall soil moisture content in the Elmendorf AFB MESL possibly from moisture entering through the single layer polyethylene sidewalls which were not treated with asphalt emulsion. There is good evidence that the membrane of the same section might have received damage during a soil sampling operation which allowed localized moisture infiltration. A two-layer polyethylene membrane used in the Ft. Wainwright MESL is considered a more positive moisture barrier than the single sheet and a justifiable added cost for permanent construction.
    Type of Medium: Series available for loan
    Pages: v, 27 Seiten , Illustrationen
    Series Statement: CRREL Report 79-16
    Language: English
    Note: CONTENTS Preface Introduction Laboratory studies General Elmendorf AFB silty clay Fairbanks silt Field studies Elmendorf AFB MESL Ft. Wainwright MESL Traffic use Elmendorf AFB MESL Ft. Wainwright MESL Performance observations Elmendorf AFB MESL Ft. Wainwright MESL Conclusions Elmendorf AFB MESL Ft. Wainwright MESL General Literature cited Appendix A. The MESL concept Appendix B. Classification, compaction, freezing and CBR test results for Fairbanks silt
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  • 56
    Call number: MOP 44440 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 105 Seiten , Illustrationen , 27 cm
    Language: English
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  • 57
    Call number: MOP 40704 / Mitte
    Type of Medium: Monograph available for loan
    Pages: VI, 35 Seiten
    Language: English
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  • 58
    Call number: AWI G3-24-95571-7
    In: Tektonika Sibiri, Tom 7
    Description / Table of Contents: Сборник включает доклады участников юбилейной Х сессии Научного совета по тектонике Сибири и Дальнего Востока, посвященной 50-летию образования Бурятской АССР и состоявшейся в г. Улан-Удэ. Тематика сборника многопланова. В обобщающих докладах рассмотрены главнейшие итоги развития научных и практических геологических исследований в Бурятской АССР. В других докладах результаты изучения разновозрастных тектонических структур Забайкалья и Прибайкалья (докембрийских, палеозойских и мезозойских), обсуждены особенности Байкальской рифтовой зоны и ее аналогов, большое внимание уделено разломам и связанным с ними магматизму и металлогении. В ряде докладов проведен сравнительный анализ тектоники Забайкалья и других регионов Азии, в частности северо - востока СССР, Монгольской Народной Республики и других территорий. Авторами использованы различные геологические и геофизические методы, включая экспериментальные. Сборник логически продолжает серию крупных работ по тектонике Сибири и Дальнего Востока, в которой уже издано шесть томов.
    Description / Table of Contents: Translation of the abstract: The collection includes reports from participants in the tenth anniversary session of the Scientific Council on Tectonics of Siberia and the Far East, dedicated to the 50th anniversary of the formation of the Buryat Autonomous Soviet Socialist Republic and held in Ulan-Ude. The collection's themes are multifaceted. The summary reports examine the most important results of the development of scientific and practical geological research in the Buryat Autonomous Soviet Socialist Republic. In other reports, the results of studying tectonic structures of Transbaikalia and Cisbaikalia of different ages (Precambrian, Paleozoic and Mesozoic), the features of the Baikal rift zone and its analogues were discussed, much attention was paid to faults and associated magmatism and metallogeny. A number of reports carried out a comparative analysis of the tectonics of Transbaikalia and other regions of Asia, in particular the northeast of the USSR, the Mongolian People's Republic and other territories. The authors used various geological and geophysical methods, including experimental ones. The collection logically continues the series of major works on the tectonics of Siberia and the Far East, in which six volumes have already been published.
    Type of Medium: Monograph available for loan
    Pages: 262 Seiten , Illustrationen
    Series Statement: Tektonika Sibiri / Akademija Nauk SSSR, Sibirskoe Otdelenie, Naučnyj Sovet po Tektonike Sibiri i Dalʹnego Vostoka Tom 7
    Language: Russian
    Note: CONTENTS INTRODUCTION TECTONICS OF TRANSBAIKAL AND ADJACENT TERRITORIES The main results and tasks of geological service of Buryat ASSR / A.S. Filko, P.Ch. Shobogorov, V.A. Lbov The state and perspectives of development of the Earth's sciences in Buryat ASSR / G.V. Andreev, V.V. Zolotukhin, Ts.O. Ochirov. The main problems of tectonics of Transbaikalje / l.V. Luchitsky The pecularities of the tectonics evolucion's style of Sayan-Baikal mountain folded belt (on territory of Buryat ASSR) / V.P. Arsentyev, P.M. Khrenov. On structural position of Transhaikal in the Middle-Asian transcontinental mobile belt / Ts.O. Ochirov On nature of mosaic structure of Transbaikal / E.N. Altukhov The continental Mesosoic structures of Transbaikal / Ts.O. Ochirov, K.B. Bulnaev, V.I. Turunkhaev, Ts.Ts. Tsyrendorzhiev Some regularities of development of Earth crust's structure of south territory of Eastern Siberia in Pre-Cambrian and Lower Paleozoic / S.M.Zamaraev, A.M. Mazukabzov, E.P. Vasilyev, A. T. Sezko The main features of evolution of tectonic magmatic stages of North Prebaikal / V. V. Balkhanov Tectonic structure and development of North territory of Baikal mountains in Late Pre-Cambrian and Early Paleozoic / S.A. Gurulev Influence of Pre-Cambrien North Muja block on sedimentation in Early and Middle Cambrian / B.A. Dalmatov, M.M.Yazmir On distinguishing of subzones in Gida Early Paleozoic structural-formation zone / M.M. Yazmir Tectonic structures of Khilok structural-formation zone (Western Transbaikal) / V.l. Sizykh Middle and Upper Paleozoic outgeosyncline magmatism of Sayan-Baikal mountain region / I. V. Gordienko Role of granitoids in reconstruction of paleotectonic condition (examplified by Transbaikal) / V.A. Dvorkin-Samarsky Principles of systematics and study of deep faults of south part of Siberian platform's frame / V.G. Gladkov, V.A. Naumov, V.l. Sizykh Magmatism of boundary sutures of Siberian platform in Middle Proterozoic / A.A. Bukharov Faults of Sayan-Baikal mountain region and some problems of its study / Ts.O. Ochirov, S.I. Sherman, V.F. Erkhov Structural-formation complexes of deep faults and rumple zones (Baikal mountain region) / M.P. Lobanov, I.A. Okhotnikov The deep faults of Transbaikal and its reflections in geophysical fields / Ts. Ts. Tsyrendorzhiev Faults of Baikal-Patom Upland according to geological-geophysical data / Yu.I. Egorov. Tectonics and metallogeny of Buryat ASSR / P.Ch. Shobogorov, A.S. Filko, V.V. Levitsky The deep faults are the main ore-controling structures of Western Baikalian rare-mecall province / E.E. Baturina Sayan-Transbaikalian poligonal system of ore-belts / V. V. Levitsky GENERAL QUESTIONS OF DEVELOPMENT OF GEOLOGICAL STRUCTURES Problems of postgeosyncline tectonic development of Central Asian folded belt / A.L. Yanshin Geosyncline folded structures of the Mongolian People's Republic / N.S. Zaitsev, The main features of tectonics of central zone of Eastern Mongolia as region of Mesozoic Tectonic-magmatic stirring up / V. T. Grigorov Pre-Cambrian tectonics of Ural-Mongolian belt and the problem of paleooceans / L.M. Parfyonov, V.A. Popeko Problem of "foundation" of Baikalian folded region / K.A. Klitin Orogenic stage of baikalids and time of its formation / A.N. Bulgatov The main features of tectonics of caledonides of South Siberia / A.L. Dodin Outgeosyncline collapse depressions of South Siberia and methodological aspects of its study / V.S. Bochkarev Minor structural forms of metamorphic strata of Eastern Transbaikal and of South Ural / V.I. Gromin The main features of structure and development of orogenic regions of North-Eastern Asia / K.B. Mokshantsev Some physical regularities of formation of Earth crust's faults / S.I. Sherman Recent Earth crust's movements in south part of Baikalian rift zone and in adjacent regions / P.P. Kolmogorova, B.G. Kolmogorov The peculiarities of structure of recent and ancient rift zones / V.V. Fedynsky, A.G. Gainanov, B.A. Sokolov, N.A. Strakhova Role of wave movements in formation of tectonic structures of South Siberian boundary system / V.G. Gladkov , СОДЕРЖАНИЕ ПРЕДИСЛОВИЕ ТЕКТОНИКА ЗАБАЙКАЛЬЯ И СМЕЖНЫХ ТЕРРИТОРИЙ Основные итоги и задачи геологоразведочной службы Бурятской АССР / А. С. Филько, П. Ч. Шобогоров, В. А. Лбов, Состояние и перспективы развития наук о Земле в Бурятской АССР / Г. В. Андреев, В. В. Золотухин, Ц. О. Очиров Основные проблемы тектоники Забайкалья / И. В. Лучицкий Особенности стиля тектонической эволюции Саяно-Байкальского горно-складчатого пояса (в пределах Бурятской АССР) / В. П. Арсентьев, П. М. Хренов О структурном положении Забайкалья в Срединно-Азиатском трансконтинентальном подвижном поясе / Ц. О. Очиров О природе мозаичности структурного плана Забайкалья / Е. Н. Алтухов Континентальные структуры мезозоя Забайкалья / Ц. О. Очиров, К. Б. Булнаев, В. И. Турунхаев, Ц. Ц. Цырендоржиев Некоторые закономерности развития структуры земной коры юга Восточной Сибири в докембрии и нижнем палеозое / С. М. Замараев, А. М. Мазукабзов, Е. П. Васильев, А. И. Сезько Основные черты эволюции тектоно-магматических этапов Северного Прибайкалья / В. В. Балханов Тектоническое строение и развитие северной части Байкальской горной области в позднем докембрии и раннем палеозое / С. А. Гурулев Влияние докембрийской Северо-Муйской глыбы на осадконакопление в раннем и среднем кембрии / Б. А. Далматов, М. М. Язмир К выделению подзон в Джидинской раннепалеозойской структурно-формационной зоне / М. М. Язмир Тектонические структуры Хилокской структурно-формационной зоны (Западное Забайкалье) / В. И. Сизых Средне- и верхнепалеозойский внегеосинклинальный магматизм Саяно-Байкальской горной области / И. В. Гордиенко Роль гранитоидов в восстановлении палеотектонической обстановки (на примере Забайкалья) / В. А. Дворкин- Самарский Принципы, систематики и изучения глубинных разломов южного обрамления Сибирской платформы / В. Г. Гладков, В. А. Наумов, В. И. Сизых Магматизм краевых швов Сибирской платформы в среднем протерозое / А. А. Бухаров Разломная тектоника Саяно-Байкальской горной области и некоторые проблемы ее изучения / Ц. О. Очиров, С. И. Шерман, В. Ф. Ерхов Структурно-формационные комплексы глубинных разломов и зон смятий (Байкальская горная область) / М. П. Лобанов, И. А. Охотников Глубинные разломы Забайкалья и их отражение в геофизических полях / Ц. Ц. Цырендоржиев Разрывная тектоника Байкало-Патомского нагорья в свете геолого-геофизических данных / Ю. И. Егоров Тектоника и металлогения Бурятской АССР / П. Ч. Шобогоров, А . С. Филько, В. В. Левицкий Глубинные разломы - главные рудоконтролирующие структуры Западно-Забайкальской редкометальной провинции / Е. Е. Батypина Саяно-Забайкальская решетчатая система рудных поясов / В. В. Левицкий ОБЩИЕ ВОПРОСЫ РАЗВИТИЯ ГЕОЛОГИЧЕСКИХ СТРУКТУР Проблемы постгеосинклинальноrо тектонического развития Центрально-Азиатского складчатого пояса / А. Л Яншин Геосииклинальные складчатые структуры МНР / Н. С. Зайцев Основные черты тектоники Центральной зоны Восточной Монголии как области мезозойской тектоно-маrматической активизации / В. Т. Григоров Докембрийская тектоника Урало-Монгольского пояса и проблема палеоокеанов / Л. М. Парфенов, В. А. Попеко Проблема "фундамента" Байкальской складчатой области / К. А . Клитин Орогенный ярус байкалид и время его формирования / А. Н. Булгатов Основные черты тектонического строения каледонид юга Сибири / А. Л. Додин Внегеосинклинальные впадины обрушения юга Сибири и методологическне аспекты их изучения / В. С. Бочкарев Малые структурные формы метаморфических толщ Восточного Забайкалья и Южного Урала / В. И. Громин Основные черты строения и развития орогенных областей северо-востока Азии / К. Б. Мокшанцев Некоторые физические закономерности формирования сети разломов земной коры / С. И. Шерман Современные движения земной коры в южной части Байкальской рифтовой зоны и в сопредельных областях / П. П. Колмогорова, В. Г. Колмогоров Особенности строения современных и древних рифтовых зон / В. В. Федынский, А. Г. Гайнанов , Б. А . Соколов, Н. А. Страхова Роль волновых движений в формировании тектонических структур Южно-Сибирской краевой системы / В. Г. Гладков , In kyrillischer Schrift
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  • 59
    Monograph available for loan
    Monograph available for loan
    Moskva : Izdatel'stvo "Nauka"
    Call number: AWI G2-24-95716
    Description / Table of Contents: Сборник включает материалы симпозиума "Поздиечетвертичная история и седиментогенез окраинных и внутренних морей", проведенного Океанографической комиссией АН СССР в 1977 г. На симпозиуме были рассмотрены результаты исследований последних лет в области стратиграфии и литологии четвертичных осадков морей СССР и шельфовой зоны Мирового океана, поздиечетвертичная история южных и дальневосточных морей СССР и некоторых морей европейского Севера. Сборник представляет интерес для геологов-четвертичников, географов, литологов, океанологов, морских геоморфологов и геологов.
    Description / Table of Contents: Translation of abstract: The collection includes materials from the symposium “Late Quaternary history and sedimentogenesis of marginal and inland seas”, held by the Oceanographic Commission of the USSR Academy of Sciences in 1977. The symposium examined the results of recent research in the field of stratigraphy and lithology of Quaternary sediments of the seas of the USSR and the shelf zone of the World Ocean, the late Quaternary history of the southern and the Far Eastern seas of the USSR and some seas of the European North. The collection is of interest to Quaternary geologists, geographers, lithologists, oceanologists, marine geomorphologists and geologists.
    Type of Medium: Monograph available for loan
    Pages: 211 Seiten , Illustrationen , 2 Kartenbeilagen
    Language: Russian
    Note: СОДЕРЖАНИЕ Особенности седиментогенеза на континентальных окраинах океанов и во внутренних морях / Ф. А. Щербаков Строение плиоцен-четвертичной толщи дна Баренцева моря на разрезе полуостров Рыбачий - острова Земля Франца-Иосифа / А. И. Блажчишин, Т. И. Линькова, О. В. Кириллов, Е. П. Шкатов К палеогеографии Баренцева моря в позднеледниковье и голоцене / Б. Н. Котенев Эволюция осадконакопления в прибрежных районах Баренцева и Белого морей в поздне- и послеледниковое время / В. Я. Евзеров Стратиграфия верхнечетвертичных отложений северной части Белого моря / Р. Н. Джиноридзе, Е. А. Кириенко, Л. В. Калугина, А. Е. Рыбалко, М. А. Спиридонов, Е. А. Спиридонова Палинологический и диатомовый анализ донных отложений Балтийского моря / Г. И. Клейменова, В. И. Хомутова, Е. М. Вишневская Стратиграфия позднечетвертичных отложений Черного моря / Ф. А. Щербаков, Е. В. Коренева, Э. К. Забелина Палеогеография Черноморского бассейна в позднечетвертичное время по данным палинологического анализа глубоководных отложений / А. В. Комаров Особенности седиментогенеза в морских подводных каньонах кавказского шельфа Черного моря / К. И. Джанджгава Об изменении биопродуктивности вод Черного моря в голоцене / Н. М. Андреева, Б. Н. Котенев, Л. Н. Розов Закономерности формирования и распределения водно-физических свойств глубоководных осадков Черного моря / В. А. Емельянов, А. Ю. Митропольский Геологическая история Керченского пролива в позднечетвертичное время / Е. Ф. Шнюков, В. М. Аленкин, А. В. Григорьев, А. Л. Путь, Н. А. Ломаев Отражение глубинных структур в морских четвертичных отложениях центральной части Азовского моря / В. Н. Семененко, О. Г. Сиденко Марганцеворудный процесс в позднем антропогене Азово-Черноморского бассейна / Г. Н. Орловский Палеоклиматы, водный баланс и уровни Черного и Каспийского морей в позднем плейстоцене-голоцене / И. Г. Авенариус Гипотетическая климатическая кривая основных этапов осадконакопления Каспийского моря в позднем плейстоцене / В.К Шкатова Процессы седиментогенеза в море Леванта / А. А. Мусса, А. Ю. Митропольский Петрографо-минералогическая характеристика современных отложений Бенгальского залива и Андаманского моря / Д. Е. Гершанович, А. И. Конюхов, И. А.Назаревич Терригенно-минералогические провинции прибрежно-шельфовой зоны Западного Индостана / О. К. Тареева Морфотектоника материкового побережья юга Дальнего Востока и морские трансгрессии позднего плейстоцена-голоцена / А. П. Кулаков Последние этапы голоценовой трансгрессии в бассейнах Японского и Охотского морей / А. М. Короткий, П. Ф. Бровко, И. И. Задкова, В. С. Пушкарь, И. Г. Шахгельдян Основные черты геологического строения шельфа и материкового склона Японского моря у побережья СССР / И. И. Берсенев, И. К. Пущин Четвертичные отложения шельфа Южного приморья на примере залива Петра Великого (Японское море) / Ю. Д. Марков Позднеnлейстоценовые бассейны Юго-Западной Камчатки и их связь с неотектоническими движениями / Р. Б. Крапивнер Криолитозона арктического шельфа Азии / З. Н. Антипина, Ф. Э. Арэ, В. В. Войченко, E. H. Молочушкин Опыт количественной оценки голоценовых тектонических движений в области шельфа / Н. Н. Дунаев Об использовании метода измерения магнитной восприимчивости морских осадков для восстановления условий их формирования на шельфе / Ю. В. Кочемасов , Translation of Table of Contents Features of sedimentogenesis on the continental margins of the oceans and in inland seas / F. A. Shcherbakov Structure of the Pliocene-Quaternary strata of the Barents Sea bottom in the section of the Rybachy Peninsula - Franz Josef Land Islands / A. I. Blazhchishin, T. I. Linkova, O. V. Kirillov, E. P. Shkatov On the paleogeography of the Barents Sea in the Late Glacial and Holocene / B. N. Kotenev Evolution of sedimentation in the coastal areas of the Barents and White Seas in late and post-glacial times / V. Ya. Evzerov Stratigraphy of Upper Quaternary sediments of the northern part of the White Sea / R. N. Dzhinoridze, E. A. Kiriyenko, L. V. Kalugina, A. E. Rybalko, M. A. Spiridonov, E. A. Spiridonova Palynological and diatom analysis of bottom sediments of the Baltic Sea / G. I. Kleimenova, V. I. Khomutova, E. M. Vishnevskaya Stratigraphy of Late Quaternary sediments of the Black Sea / F. A. Shcherbakov, E. V. Koreneva, E. K. Zabelina Paleogeography of the Black Sea basin in the late Quaternary according to palynological analysis of deep-sea sediments / A. V. Komarov Features of sedimentogenesis in marine underwater canyons of the Caucasian shelf of the Black Sea / K. I. Dzhandzhgava On changes in the bioproductivity of the Black Sea waters in the Holocene / N. M. Andreeva, B. N. Kotenev, L. N. Rozov Regularities of formation and distribution of water-physical properties of deep-sea sediments of the Black Sea / V. A. Emelyanov, A. Yu. Mitropolsky Geological history of the Kerch Strait in the late Quaternary / E. F. Shnyukov, V. M. Alenkin, A. V. Grigoriev, A. L. Put, N. A. Lomaev Reflection of deep structures in marine Quaternary sediments of the central part of the Azov Sea / V. N. Semenenko, O. G. Sidenko Manganese ore process in the late Anthropogene of the Azov-Black Sea basin / G. N. Orlovsky Paleoclimates, water balance and levels of the Black and Caspian Seas in the Late Pleistocene-Holocene / I. G. Avenarius Hypothetical climate curve of the main stages of sedimentation of the Caspian Sea in the Late Pleistocene / V.K Shkatova Processes of sedimentogenesis in the Levant Sea / A. A. Mussa, A. Yu. Mitropolsky Petrographic-mineralogical characteristics of modern sediments of the Bay of Bengal and the Andaman Sea / D. E. Gershanovich, A. I. Konyukhov, I. A. Nazarevich Terrigenous-mineralogical provinces of the coastal-shelf zone of Western Hindustan / O. K. Tareeva Morphotectonics of the continental coast of the south of the Far East and marine transgressions of the late Pleistocene-Holocene / A. P. Kulakov The last stages of the Holocene transgression in the basins of the Sea of Japan and the Sea of Okhotsk / A. M. Korotkiy, P. F. Brovko, I. I. Zadkova, V. S. Pushkar, I. G. Shakhgeldyan Main features of the geological structure of the shelf and continental slope of the Sea of Japan off the coast of the USSR / I. I. Bersenev, I. K. Pushchin Quaternary sediments of the Southern Primorye shelf using the example of Peter the Great Bay (Sea of Japan) / Yu. D. Markov Late Leistocene basins of Southwestern Kamchatka and their connection with neotectonic movements / R. B. Krapivner Cryolithozone of the Arctic shelf of Asia / Z. N. Antipina, F. E. Are, V. V. Voichenko, E. H. Molochushkin Experience in quantitative assessment of Holocene tectonic movements in the shelf area / N. N. Dunaev On the use of the method of measuring the magnetic susceptibility of marine sediments to restore the conditions of their formation on the shelf / Yu. V. Kochemasov , In kyrillischer Schrift
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  • 60
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    Monograph available for loan
    Geneva : World Meteorological Organization
    Associated volumes
    Call number: MOP Per 840(1)
    In: Marine meteorology and related oceanographic activities
    Type of Medium: Monograph available for loan
    Pages: 39 S. : Ill.
    Series Statement: Marine meteorology and related oceanographic activities 1
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  • 61
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    Monograph available for loan
    Canberra, Austr. : Canberra reprographic printers
    Call number: AWI Atl-10-0058
    Type of Medium: Monograph available for loan
    Pages: div. S.
    Edition: Ed. 4
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  • 62
    Call number: MOP Per 334/D
    Type of Medium: Monograph available for loan
    Parallel Title: Zugl. einzelne Bd. von: United States / National Oceanic and Atmospheric Administration: NOAA technical report / ERL
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  • 63
    Call number: MOP Per 607(216)
    In: Trudy
    Type of Medium: Monograph available for loan
    Pages: 130 S.
    Series Statement: Trudy / Gidrometeorologičeskij Naučno-Issledovatel'skij Centr SSSR 216
    Language: Russian
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  • 64
    Call number: MOP 45718
    In: Meteorologisches Institut der Universität Bonn
    Type of Medium: Monograph available for loan
    Pages: 83, xv S. : graph. Darst.
    Series Statement: Meteorologisches Institut der Universität Bonn 102
    Note: Bonn, Univ., Diplomarbeit, 1979
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  • 65
    Call number: MOP B 17467
    In: The Institute of Mathematics and its applications conference series : N.S.
    Type of Medium: Monograph available for loan
    Pages: XVI, 500 S.: graph. Darst.
    Series Statement: The Institute of Mathematics and its applications conference series : N.S.
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  • 66
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    Monograph available for loan
    Wellington : Govt. Print.
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    Call number: MOP Per 284(93)
    In: Meteorological Office note
    Type of Medium: Monograph available for loan
    Pages: S. 315-318
    Series Statement: Meteorological Office note 93
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  • 67
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    Monograph available for loan
    Thessaloniki : Meteorological Institute of the University of Thessaloniki
    Associated volumes
    Call number: MOP Per 736(63)
    In: Meteorologika
    Type of Medium: Monograph available for loan
    Pages: p. 357-420, [1] : ill.
    Series Statement: Meteorologika 63
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  • 68
    Call number: MOP Per 701/B(NF, 10)
    In: Meteorologische Abhandlungen
    Type of Medium: Monograph available for loan
    Series Statement: Meteorologische Abhandlungen : Serie B, Grundlagenmaterial N. F., 10
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  • 69
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    Monograph available for loan
    Warszawa : Polish Scient. Publ.
    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
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  • 70
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    Call number: MOP Per 225(31)
    In: Ergebnisse der aerologischen und bodennahen Ozonmessungen im ...
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    Series Statement: 31
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  • 71
    Monograph available for loan
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    s.l.
    Call number: MOP S 12236
    Type of Medium: Monograph available for loan
    Pages: 34 S.
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  • 72
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    Call number: MOP 39349/6
    In: Mirovaja naučnaja i techničeskaja Literatura
    Type of Medium: Monograph available for loan
    Pages: 321 S.
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  • 73
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    Delhi : Manager of Publ., Civil Lines ; 26.1975 - 29.1978
    Call number: MOP Per 56
    Type of Medium: Monograph available for loan
    ISSN: 0376-4796
    Former Title: Vorg. ---〉 Indian journal of meteorology & geophysics
    Subsequent Title: Forts. ---〉 Mausam
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  • 74
    Call number: MOP Per 800(431)
    In: WMO
    In: Technical note
    Type of Medium: Monograph available for loan
    Pages: 27 S.
    ISBN: 926310431X
    Series Statement: WMO / World Meteorological Organization 431
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  • 75
    Call number: MOP 22993
    In: Nastavlenie gidrometeorologicheskim stancijam i postam
    Type of Medium: Monograph available for loan
    Pages: 239 S.
    Series Statement: Nastavlenie gidrometeorologicheskim stancijam i postam 10, 1
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  • 76
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    Tokyo : National Institute of Polar Research
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    Call number: ZSP-592-13
    In: Memoirs of National Institute of Polar Research
    Type of Medium: Series available for loan
    Pages: IV, 245 S. : Ill., graph. Darst.
    Series Statement: Memoirs of National Institute of Polar Research : Special issue 13
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  • 77
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    Moskva [u.a.] : Akad.
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    Call number: MOP Per 324(106)
    In: Trudy Instituta Okeanologii
    Type of Medium: Monograph available for loan
    Pages: 178 S.
    Series Statement: Trudy Instituta Okeanologii 106
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  • 78
    Call number: S 12.0222(65)
    In: Acta phytogeographica Suecica
    Type of Medium: Series available for loan
    Pages: 121 S. : Ill., graph. Darst., Kt.
    ISBN: 9172100656 , 91-7210-465-1
    Series Statement: Acta phytogeographica Suecica 65
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    Tokyo : National Institute of Polar Research
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    Call number: ZSP-592-12
    In: Memoirs of National Institute of Polar Research
    Type of Medium: Series available for loan
    Pages: I, 282 S. : Ill., graph. Darst., Kt.
    Series Statement: Memoirs of National Institute of Polar Research : Special issue 12
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    Call number: S 12.0222(66)
    In: Acta phytogeographica Suecica
    Type of Medium: Series available for loan
    Pages: 120 S. : Ill.
    ISBN: 9172100664 , 91-7210-466-X
    Series Statement: Acta phytogeographica Suecica 66
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 81
    Monograph available for loan
    Monograph available for loan
    Zürich : Inst. Suisse de Météorologie
    Associated volumes
    Call number: MOP Per 24(35)
    In: Veröffentlichungen der Schweizerischen Meteorologischen Zentralanstalt
    Type of Medium: Monograph available for loan
    Pages: vii, 102 p. : ill.
    Series Statement: Veröffentlichungen der Schweizerischen Meteorologischen Zentralanstalt 35
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 82
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP Per 666(6,1)
    In: GATE
    Type of Medium: Monograph available for loan
    Pages: 32 S. : Ill., graph. Darst.
    Series Statement: 6,1
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 83
    Monograph available for loan
    Monograph available for loan
    Offenbach, M : Dt. Wetterdienst
    Associated volumes
    Call number: MOP Per 666(6,4)
    In: Promet
    Type of Medium: Monograph available for loan
    Pages: 32 S. : graph. Darst.
    Series Statement: Promet 6,4
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 84
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP 44219
    In: Einführung in die mathematische Statistik
    Type of Medium: Monograph available for loan
    Pages: 396 S. : Ill.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 85
    Monograph available for loan
    Monograph available for loan
    Leningrad [u.a.] : Gidrometeorog. Izd-vo
    Associated volumes
    Call number: MOP Per 377(173) ; MOP Per 377(173, 2. Ex.)
    In: Trudy Ukrainskogo Naučno-Issledovatel'skogo Gidrometeorologičeskogo Instituta
    Type of Medium: Monograph available for loan
    Pages: 159 S.
    Series Statement: Trudy Ukrainskogo Naučno-Issledovatel'skogo Gidrometeorologičeskogo Instituta 173
    Location: MOP - must be ordered
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 86
    Call number: MOP Per 807(3)
    In: Precipitation Enhancement Project report
    Type of Medium: Monograph available for loan
    Pages: 38, [5] p.
    Series Statement: Precipitation Enhancement Project report 3
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 87
    Call number: MOP Per 29/D(107)
    In: NOAA technical memorandum
    Type of Medium: Monograph available for loan
    Pages: VII, 73 S.
    Series Statement: NOAA technical memorandum : NESS 107
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 88
    Monograph available for loan
    Monograph available for loan
    Geneva : Secretariat of the World Meteorological Organization
    Associated volumes
    Call number: MOP Per 800(530) ; MOP Per 800(530, 2. Ex.)
    In: WMO
    In: Technical note
    Type of Medium: Monograph available for loan
    Pages: 201 S. : Ill.
    ISBN: 9263105308
    Series Statement: WMO / World Meteorological Organization 530
    Location: MOP - must be ordered
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 89
    Monograph available for loan
    Monograph available for loan
    Leningrad : Gidrometeoizdat
    Associated volumes
    Call number: MOP Per 283(415)
    In: Trudy
    Type of Medium: Monograph available for loan
    Pages: 118 S.
    Series Statement: Trudy / Glavnaja Geofiziceskaja Observatorija Imeni A. I. Voejkova 415
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 90
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: MOP 44629(1974-1975) / Mitte
    In: Obščee soderžanie atmosfernogo ozona i spektral'naja prozračnost' atmosfery
    Type of Medium: Monograph available for loan
    Pages: 339 S.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 91
    Monograph available for loan
    Monograph available for loan
    Geneva : Secretariat of the World Meteorological Organization
    Associated volumes
    Call number: MOP Per 800(442) ; MOP Per 800(442, 2. Ex.)
    In: WMO
    Type of Medium: Monograph available for loan
    Pages: 112 S. : Ill.
    Series Statement: WMO / World Meteorological Organization 442
    Location: MOP - must be ordered
    Location: MOP - must be ordered
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 92
    Monograph available for loan
    Monograph available for loan
    Obninsk : Informacionnyj centr
    Call number: MOP 40427
    Type of Medium: Monograph available for loan
    Pages: 25 S.
    Series Statement: Obzor : serija avtomatizacija sbora i obrabotki gidrometeorologičeskoj informacii
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 93
    Call number: K-13-0019(1-6)
    Pages: 1 Kt. in 6 Bl. : mehrfarb.
    Branch Library: AWI Library
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  • 94
    Call number: MOP 40918(9) / Mitte
    In: The Nimbus 6 data catalog
    Type of Medium: Monograph available for loan
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 95
    Call number: AWI G7-84-0848
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 127 S.
    Branch Library: AWI Library
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  • 96
    Monograph available for loan
    Monograph available for loan
    Berlin : Duncker & Humblot
    Associated volumes
    Call number: MOP 44510
    In: Studien aus dem Institut für Internationales Recht an der Universität Kiel
    Type of Medium: Monograph available for loan
    Pages: XIII, 174 S.
    ISBN: 3428035623
    Series Statement: Studien aus dem Institut für Internationales Recht an der Universität Kiel 1
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 97
    Call number: ZSP-594/C-9
    In: Memoirs of National Institute of Polar Research
    Type of Medium: Series available for loan
    Pages: 41 S. : graph. Darst., Ill.
    Series Statement: Memoirs of National Institute of Polar Research : Series C, Earth Sciences 9
    Branch Library: AWI Library
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  • 98
    Call number: AWI G7-84-0849
    In: Katalog dannych i publikacij po Arktike i Antarktike
    Type of Medium: Monograph available for loan
    Pages: 86 S.
    Branch Library: AWI Library
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  • 99
    Monograph available for loan
    Monograph available for loan
    Reading ; 1979 - 1986 nachgewiesen
    Call number: MOP 45206
    Type of Medium: Monograph available for loan
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 100
    Monograph available for loan
    Monograph available for loan
    Moskva : Mosk. Otdel. Gidromet.
    Call number: MOP 44801 / Mitte
    Type of Medium: Monograph available for loan
    Pages: 29 S.
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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