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  • 1
    Series available for loan
    Series available for loan
    Associated volumes
    Call number: ZSP-164-26
    In: The Geology of the South Shetland Islands
    Description / Table of Contents: King George Island is almost entirely composed of igneous rocks; four volcanic episodes and one intrusive phase are represented. The oldest volcanics, which are believed to be Upper Jurassic in age, form a calc-alkaline suite with an andesite-rhyolite association. Recent field investigations indicate there is no evidence for the extensive areas of sedimentary rocks previously recorded. The presence of regionally metamorphosed xenoliths in the Jurassic Volcanos indicates that they rest upon a Basement Complex. The early Tertiary Andean Intrusive Suite, which is petrographically similar to that of Graham Land, forms an axial core to the island. The majority of the Jurassic Volcanics have been metasomatized by these intrusions and the significance of the resultant secondary minerals is discussed. A linear pattern of Tertiary and Quaternary vulcanicity has been demonstrated and lavas of three distinct episodes are described. One of these volcanic groups is of unknown age, whilst the others are known to be Middle Miocene and Recent. The lavas include dominant pyroxene-andesites, basaltic andesites, olivine-basalts and rare trachyandesites. The petrogenesis of the volcanic site is discussed and crystal separation is suggested as the most important factor in their evolution. A geological map, compiled from all the available rock collections and field notes, shows the distribution of the volcanic and intrusive groups.
    Type of Medium: Series available for loan
    Pages: 28 S. : Ill., Kt.
    Series Statement: 26
    Branch Library: AWI Library
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  • 2
    Call number: ZSP-697/B
    Parallel Title: 2=2; 3=3; 10=5a von [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / 12 / Sejsmologiceskie issledovanija]
    Subsequent Title: Forts. ---〉 [Rezul'taty issledovanij po mezdunarodnym geofiziceskim proektam / Gljaciologija]
    Location: AWI Reading room
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  • 3
    Call number: AWI E2-13-0068-2
    In: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda, Tom 2
    Type of Medium: Monograph available for loan
    Pages: 653 Seiten
    Series Statement: Materialy nabljudenij naučno-issledovatel'skich drejfujuščich stancij "Severnyj Poljus-6", "Severnyj Poljus-7" 1957/58 goda 2
    Language: Russian
    Note: СОДЕРЖАНИЕ = Soderžanie = Contents: Предисловие = Predislovie = Foreword. - Метеорология = Meteorologija = Meteorology. - Метеорологические наблюдения = Meteorologičeskie nabljudenija = Meteorological observations. - Таблицы = Tablicy = Tables. - Актинометрия = Aktinometrija = Actinometry. - Актинометрические наблюдения = Aktinometričeskie nabljudenija = Actinometric observations. - Некоторые результаты наблюдений = Nekotorye rezul'taty nabljudenij = Some results of observations. - Таблицы = Tablicy = Tables. - , In kyrillischer Schrift
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  • 4
    Monograph available for loan
    Monograph available for loan
    Associated volumes
    Call number: AWI G7-92-0551
    In: Gljaciologiceskie issledovanija v period MGG
    Type of Medium: Monograph available for loan
    Pages: 233 S. : Ill., Kt.
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  • 5
    Series available for loan
    Series available for loan
    Oslo : Univ. Press [in Komm.]
    Associated volumes
    Call number: ZSP-597-123
    In: Skrifter
    In: Scientific results
    Type of Medium: Series available for loan
    Pages: 47 S
    Series Statement: Skrifter / Norsk Polarinstitutt 123
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  • 6
    Call number: ZSP-164-27
    In: The Geology of the South Shetland Islands
    Description / Table of Contents: Decption Island is a caldera formed by the subsidence of a group of overlapping volcanoes along arcuate and radial faults. Three volcanic episodes occured after the formation of the caldera and the location of those post-caldera volcanoes is controlled by the fault pattern which limits the caldera. Although it is possible to establish the relative ages of the four volcanic episodes, there is little information as to their absolute ages. It is probable that the latest eruptions occurred in historic times. Petrographically the Deception Island suite is a local alkaline deviation from the normal andesite-rhyolite association of the South Shetland Islands. Its lavas are characterized by an unusually high soda content. The sequence of crystallization is analogous to that of melts of certain composition in the system MgO-FeO-SiO2 crystallizing under conditions of strong fractionation. The geochemistry of the Deception Island volcanic rocks is reviewed and four new chemical analyses are presented.
    Type of Medium: Series available for loan
    Pages: 43 S. : Ill., graph. Darst., Kt. + 2 Kt.-Beil.
    Series Statement: 27
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  • 7
    Series available for loan
    Series available for loan
    New York : IGY World Data Center A, Glaciology
    Associated volumes
    Call number: AWI G7-85-0723
    In: IGY Glaciological Report
    Type of Medium: Series available for loan
    Pages: xiv, 197 p. : Ill.
    Series Statement: IGY Glaciological Report 5
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  • 8
    Monograph available for loan
    Monograph available for loan
    Rostock : Hinstorff
    Call number: AWI E1-93-0333
    Type of Medium: Monograph available for loan
    Pages: 233 S. : Fototaf. ; 21 cm
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  • 9
    Monograph available for loan
    Monograph available for loan
    Leipzig : Brockhaus
    Call number: AWI E3-86-0848
    Type of Medium: Monograph available for loan
    Pages: 280 S. : Fototaf. , 1 Kte. ; 24 cm
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  • 10
    Monograph available for loan
    Monograph available for loan
    New York [u.a.] : McGraw-Hill
    Call number: AWI A17-98-0088
    Type of Medium: Monograph available for loan
    Pages: XIV, 285 S. , graph. Darst.
    Note: Contents: Translator's preface. - Author's preface. - PART 1 SOME TOPICS FROM THE THEORY OF RANDOM FIELDS AND TURBULENCE THEORY. - Introductory remarks. - 1. Methods for statistical description of continuous random fields. - 1.1 Stationary random functions. - 1.2 Random functions with stationary increments. - 1.3 Homogeneous and isotropic random fields. - 1.4 Locally homogeneous and isotropic random fields. - 2. The microstructure of turbulent flow. - Introductory remarks. - 2.1 Onset and development of turbulence. - 2.2 Structure functions of the velocity field in developed turbulent flow. - 2.3 Spectrum of the velocity field in turbulent flow. - 3. Microstructure of the concentration of a conservative passive additive in a turbulent flow. - 3.1 Turbulent mixing of conservative passive additives. - 3.2 Structure functions and spectral functions of the field of a conservative passive additive in a turbulent flow. - 3.3 Locally isotropic turbulence with smoothly varying mean characteristics. - 3.4 Microstructure of the refractive index in a turbulent flow. - PART 2 SCATTERING OF ELECTROMAGNETIC AND ACOUSTIC WAVES IN THE TURBULENT ATMOSPHERE. - 4. Scattering of electromagnetic waves in the turbulent atmosphere. - Introductory remarks. - 4.1 Solution of Maxwell's equations. - 4.2 The mean intensity of scattering. - 4.3 Scattering by inhomogeneous turbulence. - 4.4 Analysis of various scattering theories. - 4.5 Evaluation of the size of refractive index fluctuations from data on the scattering of radio waves in the troposphere. - 5. The scattering of sound waves in a locally isotropic turbulent flow. - PART 3 PARAMETER FLUCTUATIONS OF ELECTROMAGNETIC AND ACOUSTIC WAVES PROPAGATING IN A TURBULENT ATMOSPHERE. - Introductory remarks. - 6. Solution of the problem of amplitude and phase fluctuations of a plane monochromatic wave by using the equations of geometrical optics. - 6.1 Derivation and solution of the equations of geometrical optics. - 6.2 The structure function and the spectrum of the phase fluctuations of the wave. - 6.3 Solution of the equations of geometrical optics by using spectral expansions. - 6.4 Amplitude and phase fluctuations of a wave propagating in a locally isotropic turbulent flow. - 6.5 A consequence of the low of conservation of energy. - 6.6 Amplitude and phase fluctuations of sound waves. - 6.7 Limits of applicability of geometrical optics. - 7. Calculation of amplitude and phase fluctuations of a plane monochromatic wave from the wave equation using the methods of "small" and "smooth" perturbations. - 7.1 Solution of the wave equation by the method of small perturbations. - 7.2 The equations of the method of smooth perturbations. - 7.3 Solution of the equations of the method of "smooth" perturbations by using spectral expansions. - 7.4 Qualitative analysis of the solutions. - 7.5 Amplitude and phase fluctuations of a wave propagating in a locally isotropic turbulent medium. - 7.6 Relation between amplitude and phase fluctuations and wave scattering. - 8. Parameter fluctuations of a wave propagating in a turbulent medium with smoothly varying characteristics. - 9. Amplitude fluctuations of a spherical wave. - PART 4 EXPERIMENTAL DATA ON PARAMETER FLUCTUATIONS OF LIGHT AND SOUND WAVES PROPAGATING IN THE ATMOSPHERE. - 10. Empirical data on fluctuations of temperature and wind velocity in the layer of the atmosphere near the earth and in the lower troposphere. - 11. Experimental data on the amplitude and phase fluctuations of sound waves propagating in the layer of the atmosphere near the earth. - 12. Experimental investigation of the scintillation of terrestrial light. - Introductory remarks. - 12.1 The probability distribution function of the fluctuations of light intensity. - 12.2 Dependence of the amount of scintillation on the distance and on the meteorological conditions. - 12.3 The correlation function of the fluctuations of light intensity in the plane perpendicular to the ray. - 12.4 Frequency spectra of the fluctuations of the logarithm of the light intensity (theory). - 12.5 Frequency spectrum of fluctuations of light intensity (experimental results). - 13. Twinkling and quivering of stellar images in telescopes. - Appendix. - Notes and remarks. - References.
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