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  • 1
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: G 9049 ; M 92.0833 ; AWI G1-98-0179
    Description / Table of Contents: Table of contents: PART I CLAY MINERALS AND WEATHERING. - Chapter 1 Clay minerals. - Chapter 2 Clay formation through weathering. - PART II CLAY SEDIMENTATION ON LAND. - Chapter 3 Deserts, glaciers, rivers. - Chapter 4 Lacustrine clay sedimentation. - PART III FROM LAND TO SEA. - Chapter 5 Estuaries and deltas. - Chapter 6 Clay sorting and settling in the ocean. - Chapter 7 Aeolian input. - Chapter 8 Terrigenous supply in the ocean. - PART IV CLAY GENESIS IN THE SEA. - Chapter 9 Alkaline, Evaporative environment. - Chapter 10 Ferriferous clay granules and facies. - Chapter 11 Organic environment. - Chapter 12 Metalliferous clay in deep sea. - Chapter 13 Hydrothermal environment. - PART V CLAY DIAGENESIS. - Chapter 14 Early processes. - Chapter 15 Depth of burial. - Chapter 16 Tectonic, lithologic and hydrothermal constraints. - PART VI CLAY STRATIGRAPHY AND PALEOENVIRONMENT. - Chapter 17 Paleoclimate expression. - Chapter 18 Paleocirculation and tectonics. - Chapter 19 Paleoenvironmental reconstruction. - Chapter 20 Clay and geodynamics. - References. - Subject Index
    Type of Medium: Monograph available for loan
    Pages: XX, 623 S. : Ill., graph. Darst.
    ISBN: 3540508899
    Language: English
    Location: Upper compact magazine
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Amsterdam [u.a.] : Elsevier
    Associated volumes
    Call number: 4/M 03.0580
    In: Developments in earth & environmental sciences
    Type of Medium: Monograph available for loan
    Pages: xxi, 527 S.
    ISBN: 0444514252
    Series Statement: Developments in earth and environmental sciences 1
    Classification: D.5.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Springer
    Call number: M 92.0836
    Type of Medium: Monograph available for loan
    Pages: X, 285 S. : 177 Ill., 17 graph. Darst.
    ISBN: 3540523766
    Uniform Title: Sedimentologie
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Study of clay sedimentation in the Tyrrhenian area during late Miocene time allows to distinguish continental, synsedimentary, and diagenetic influences on the composition of sedimentary rocks, according to the geographic location. In south Sicily smectite-rich assemblages were mainly eroded from soils developed under subarid conditions. On the eastern margin of Sardinia abundant micaillite was supplied from exposed areas tectonically rejuvenated during the opening of the Tyrrhenian Sea. In the westernmost part of the Tyrrhenian Basin evaporative environments combined to strong geothermal gradient allowed the formation of sediments rich in euhedral chlorite.
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Cretaceous to Palaeogene sedimentary series in two long, continously recovered boreholes from the Senegal coastal basin and adjacent Cape Verde deep-sea basin have been compared by mineralogical, geochemical, electron-microscope and microprobe investigations. The transition between the diagenetic influences related to the depth of burial and the palaeoenvironmental influences, identified in the thick coastal-basin successions, is complicated by the tectonic instability of the margin during periods of high subsidence rates and crustal thinning. As the deep-sea basin sediments are only slightly affected by diagenetic changes, the comparison between the deep sea and coastal series allows the relative effects of lithostatic pressure, tectonics and other palaeoenvironmental factors to be evaluated. The disappearance of synsedimentary signatures (tectonics, climate, depositional conditions, etc.) expressed by clay mineralogy occurs below 4.5 km; there are no significant diagenetic changes in sediments at less than 2 km depth. By comparing identical time slices in coastal and deep-sea basins, it is possible to recognize from the clay stratigraphic record the main African detrital sources, the hot and often semi-arid character of the continental climate during the Cretaceous, the existence of minor but extensive stages of tectonic activity (Barremian-late Aptian, late Albian-early Cenomanian), the temporary existence of semi-closed basins on the shelf (Late Cretaceous, early Palaeogene) and the complexity of transport and sedimentation relationships between proximal and distal environments.
    Type of Medium: Electronic Resource
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  • 6
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Lenôtre, Nicole; Chamley, Hervè; Hoffert, Michel (1985): Clay stratigraphy at Deep Sea Drilling Project Sites 576 and 578, Leg 86 (Western North Pacific). In: Heath GR; Burckle LH; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 86, 571-579, https://doi.org/10.2973/dsdp.proc.86.124.1985
    Publication Date: 2018-09-27
    Description: Late Cretaceous and Cenozoic sediments deposited on the eastern and western sides of the Shatsky Rise show similar clay assemblages of chlorite, illite, mixed layers, smectite, kaolinite, and palygorskite, and a similar vertical differentiation into three units. The deep-sea pelagic red clay is dominated by terrigenous components, which suggests that diagenesis is minor in this part of the western North Pacific and that eolian supply is very important. The role of the Shatsky Rise as a submarine barrier is of minor importance. The volcanic contribution to the clay component appears very small, as in some other parts of the Pacific Ocean. Stratigraphic correlations between Sites 576 and 578, which can be made from mineralogical data, partly offset the rareness of biostratigraphic markers.
    Type: Dataset
    Format: text/tab-separated-values, 247 data points
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Chamley, Hervè; Debrabant, Pierre; Candillier, Anne-Marie; Foulon, J (1983): Clay mineralogical and inorganic geochemical stratigraphy of Blake-Bahama Basin since the Callovian, Site 534, Deep Sea Drilling Project Leg 76. In: Sheridan, RE; Gradstein, FM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Govt. Printing Office), 76, 437-451, https://doi.org/10.2973/dsdp.proc.76.113.1983
    Publication Date: 2019-04-16
    Description: Mineralogical and geochemical investigations carried out on Callovian to upper Cenozoic basalt and sediments of Hole 534A are the bases for paleoenvironmental interpretations. The clay mineralogy primarily reflects events that occurred on the American continent (tectonics, morphology, alteration and pedogenesis, climate), except in the basalt and at the precise basalt/sediment contact where in situ alteration and local metamorphic effects exist. The inorganic and organic geochemistry mainly reflects the influence of and increasing distance from the spreading center during the first stages of sedimentation, the terrigenous influence from the Valanginian upward, and the bottom reducing or oxidizing conditions linked to the widening and deepening of the ocean affected by global tectonics.
    Type: Dataset
    Format: text/tab-separated-values, 1893 data points
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  • 8
    Publication Date: 2018-09-28
    Type: Dataset
    Format: text/tab-separated-values, 24 data points
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  • 9
    Publication Date: 2018-09-28
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 10
    Publication Date: 2018-09-28
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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