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  • 1990-1994  (2,430)
Collection
Keywords
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Language
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Year
  • 1
    Monograph available for loan
    Monograph available for loan
    Correlations and connectivity : Geometric aspects of physics, chemistry and biology : Proceedings of the NATO advanced study on corsica, France, 2.-14 July 1990 (1990)
    Dordrecht [u.a.] : Kluwer Acad. Publ.
    Associated volumes
    Details Availability
    Call number: PIK N 340-94-0365
    In: NATO ASI series
    Type of Medium: Monograph available for loan
    Pages: 330 p.
    ISBN: 0792310101
    Series Statement: NATO ASI series : E, Applied sciences 188
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Series available for loan
    Series available for loan
    Sedimentology of the Conglomeratic lower member of the Lospe Formation (lower Miocene), Santa Maria basin, California (1994)
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Details Availability
    Call number: SR 90.0001(1995-D,E)
    In: U.S. Geological Survey bulletin
    Type of Medium: Series available for loan
    Pages: IV, D21, E7 S.
    Series Statement: U.S. Geological Survey bulletin 1995-D,E
    Language: English
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    The impact of horizontal resolution on moist processes in the ECMWF Model (1993)
    Livermore, Californien : Lawrence Livermore National Laboratory
    Associated volumes
    Details Availability
    Call number: PIK N 456-04-0049
    In: Program for Climate Model Diagnosis and Intercomparison ; PCMDI Report
    Type of Medium: Monograph available for loan
    Pages: 36 S.
    Series Statement: Program for Climate Model Diagnosis and Intercomparison PCMDI Report
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    The environmental policy of the European communities (1992)
    London [u.a.] : Kluwer Law
    Associated volumes
    Details Availability
    Call number: PIK N 071-92-1101
    In: International environmental law and policy series
    Type of Medium: Monograph available for loan
    Pages: 349 p.
    Edition: 2. Aufl.
    ISBN: 1853332259
    Series Statement: International environmental law and policy series
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    The Earth Summit : The united nations conference on environment and development (unced) (1993)
    Graham [and] Trotman : London
    Details Availability
    Call number: PIK B 160-94-0054
    Type of Medium: Monograph available for loan
    Pages: 532 p.
    Edition: 1. Aufl.
    ISBN: 1853337846
    Series Statement: International Environmental Law and Policy ;
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 6
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    The Rocky Road to ‘Computopia’ (1992)
    American Institute of Physics
    Details
    Publication Date: 1992-01-01
    Print ISSN: 0031-9228
    Electronic ISSN: 1945-0699
    Topics: Physics
    Published by American Institute of Physics
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  • 7
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    Fractal landscapes and molecular evolution: modeling the myosin heavy chain gene family (1993)
    Cell Press
    Details
    Publication Date: 1993-12-01
    Print ISSN: 0006-3495
    Electronic ISSN: 1542-0086
    Topics: Biology , Physics
    Published by Cell Press
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  • 8
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    Clay and silica minerals of ODP Site 123-765 (1992)
    PANGAEA
    In:  Supplement to: Compton, John S; Locker, Stanley D (1992): Diagenesis of clay and silica minerals in sediments from the Argo Basin, Northeastern Indian Ocean (Site 765). In: Gradstein, FM; Ludden, JN; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 123, 57-75, https://doi.org/10.2973/odp.proc.sr.123.164.1992
    Details
    Publication Date: 2024-01-09
    Description: Sediments recovered from Site 765 can be divided into seven mineral associations, based on differences in clay mineralogy. These clay mineral associations correlate with the lithologic units and reflect the rift-to-drift history of the passive Australian margin. In general, the Lower to mid-Cretaceous sediments represent altered volcanic material and detrital aluminosilicates that were deposited during the early formation of the Argo Basin. The predominant clay mineral is randomly interstratified illite/smectite (I/S) that contains less than 10% illite layers. The transformation of smectite to illite is suggested by an increase in the percentage of illite layers in the basal sediments (from 〈10% to 40%) that corresponds to the silica transformation of opal-CT to quartz. This mixed-layered illite/smectite has an average composition of (K0.14 Na0.29 C0.07)(Al0.88 Mg0.43 Fe0.61 Ti0.06)(Si3.88 Al0.12)(O)10(OH)2. The highly smectitic composition of the I/S and its association with bentonite layers and zeolite minerals suggest that much of the I/S was derived from the alteration of volcanic material. The condensed middle to Upper Cretaceous sediments consist of palygorskite and detrital I/S that contains 30% to 60% illite layers. The condensed Paleogene sediments contain no palygorskite and are dominated by detrital clay minerals or by highly smectitic I/S associated with bentonite layers and zeolite minerals. The overlying, rapidly deposited Neogene clayey calcareous turbidites consist of three distinct clay mineral associations. Middle Miocene sediments contain palygorskite, kaolinite, and a tentatively identified mixed-layered illite/smectite/chlorite (I/S/C) or saponite. Upper Miocene sediments contain abundant sepiolite and kaolinite and lesser amounts of detrital I/S. Detrital I/S and kaolinite dominate the clay mineralogy of Pliocene and Pleistocene sediments. The fibrous, magnesium-rich clay minerals sepiolite and palygorskite appear to be authigenic and occur intimately associated with authigenic dolomite. The magnesium required to form these Mg-rich minerals was supplied by diffusion from the overlying seawater, and silica was supplied by the dissolution of associated biogenic silica.
    Keywords: 123-765B; 123-765C; DRILL; Drilling/drill rig; Joides Resolution; Leg123; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
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    (Table 1) Summary of horizon, lithology, and paleomagnetic of ODP Hole 126-791B basaltic mousse samples (1992)
    PANGAEA
    In:  Supplement to: Koyama, Masato; Cisowski, Stanley M; Gill, James B (1992): Paleomagnetic estimate of emplacement mechanisms of deep basaltic volcaniclastic rocks in the Sumisu Rift, Izu-Bonin Arc. In: Taylor, B; Fujioka, K; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 126, 371-379, https://doi.org/10.2973/odp.proc.sr.126.144.1992
    Details
    Publication Date: 2024-01-09
    Description: A paleomagnetic study was made on the highly vesiculated basaltic tuff breccia (the basaltic mousse) drilled by Ocean Drilling Program Leg 126 from the Izu-Bonin backarc, Sumisu Rift, to estimate the mode of its emplacement. Thirty-four 10-cm**3 minicore samples were collected from almost all the horizons of the basaltic mousse. Stepwise thermal and alternating-field demagnetization experiments show that the natural remanent magnetizations of many samples are mainly composed of a single stable component. Although remanence inclinations are not expected to be disturbed by rotary drilling, the measured inclinations of remanence show a random directional distribution as a whole. The remanence inclinations, however, show directional consistency on a smaller scale. High-density sampling and measurements from a limited interval of drilled cores, and the measurement of small disks cut from a single minicore sample show that there is directional consistency over several centimeters. Strong and stable remanent magnetization, the existence of remanence direction consistency, and the fresh lithology of the samples suggest the thermal origin of remanence. Combining the paleomagnetic results with other geological, petrographical, and paleontological characters, the Hole 791B basaltic mousse can be interpreted as a subaqueous explosion breccia produced by deep-sea pyroclastic fountaining.
    Keywords: 126-791B; Clastics; Demag Type; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg126; Median demagnetizing field; NRM, Declination; NRM, Inclination; NRM, Intensity; Ocean Drilling Program; ODP; Philippine Sea; Piece; Sample code/label; Sample comment; Temperature, technical
    Type: Dataset
    Format: text/tab-separated-values, 378 data points
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  • 10
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    (Table 1) Remanence properties of samples from ODP Core 126-792A-7H (1992)
    PANGAEA
    In:  Supplement to: Cisowski, Stanley M; Koyama, Masato (1992): Detailed record of the Brunhes/Matuyama polarity reversal in high sedimentation rate marine sediments from the Izu-Bonin Arc. In: Taylor, B; Fujioka, K; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 126, 341-352, https://doi.org/10.2973/odp.proc.sr.126.142.1992
    Details
    Publication Date: 2024-01-09
    Description: A combination of high sedimentation rates and high concentrations of magnetic grains in cores from Ocean Drilling Program Leg 126 resulted in the recovery of detailed direction and intensity records of the Brunhes/Matuyama geomagnetic polarity reversal. Virtual geomagnetic poles (VGPs) computed from azimuthally oriented samples taken from the cores of Hole 792A in the western Izu-Bonin forearc basin reveal that the geomagnetic pole persisted at moderate to high southern latitudes for several thousand years before a rapid migration to northern latitudes. Alternating-field demagnetization behavior, as well as NRM, NRM/ARM, and NRM/IRM intensities for samples from this same interval, and the NRM/IRM intensities derived from unoriented core samples from Holes 790C and 791B, drilled in the ~100-km distant Sumisu Rift, all suggest that the dipole field oscillated widely in intensity before the reversal. The fast polarity change occurred at the low point of an ~1100-yr field intensity cycle. This "reversal cycle" immediately followed earlier intensity cycles whose peaks rivaled or surpassed the normalized intensities of discrete samples from well above and below the reversal interval; furthermore, the troughs indicate a much diminished dipole field at their nadir.
    Keywords: 126-792A; ARM, Intensity, per unit volume; Demagnetization level; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; IRM, Intensity, per unit volume; Joides Resolution; Leg126; North Pacific Ocean; NRM, Intensity after demagnetization; NRM, Median destructive field/ARM, Median destructive field ratio; NRM, Median destructive field/IRM, Median destructive field ratio; Ocean Drilling Program; ODP; Sample code/label; Type; Virtual geomagnetic pole latitude; Virtual geomagnetic pole longitude
    Type: Dataset
    Format: text/tab-separated-values, 188 data points
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