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  • -; 74-526A; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Glomar Challenger; Leg74; Nannofossil zone; Planktic foraminifera zone; Sample code/label; South Atlantic/CREST; Traces  (1)
  • 119-745B; 119-746A; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg119; Ocean Drilling Program; ODP  (1)
  • 119-745B; Chlorite (Area, 3.54Å); Chlorite (Area, 4.7Å); Chlorite (Area, 7Å); DEPTH, sediment/rock; DRILL; Drilling/drill rig; Illite (Area, 10Å); Illite (Area, 4.5Å); Indian Ocean; Joides Resolution; Kaolinite (Area, 3.58Å); Leg119; Ocean Drilling Program; ODP; Smectite (Area, 17Å); X-ray diffraction TEXTUR, clay fraction  (1)
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  • 1
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Fütterer, Dieter K (1984): Evidence of Clionid sponges in sediments of the Walvis Ridge, southeastern Atlantic Site 526, Deep Sea Drilling Project Leg 74. In: Moore, TC Jr; Rabinowitz, PD; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 74, 557-560, https://doi.org/10.2973/dsdp.proc.74.113.1984
    Publikationsdatum: 2023-06-27
    Beschreibung: Pelagic carbonate oozes of DSDP Site 526 contain remnants of the activity of boring sponges of the family Clionidae: (1) the borings themselves = ichnogenus Entobia and (2) the characteristically shaped boring chips as a finegrained sediment component.
    Schlagwort(e): -; 74-526A; Deep Sea Drilling Project; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Epoch; Glomar Challenger; Leg74; Nannofossil zone; Planktic foraminifera zone; Sample code/label; South Atlantic/CREST; Traces
    Materialart: Dataset
    Format: text/tab-separated-values, 54 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2024-01-09
    Schlagwort(e): 119-745B; Chlorite (Area, 3.54Å); Chlorite (Area, 4.7Å); Chlorite (Area, 7Å); DEPTH, sediment/rock; DRILL; Drilling/drill rig; Illite (Area, 10Å); Illite (Area, 4.5Å); Indian Ocean; Joides Resolution; Kaolinite (Area, 3.58Å); Leg119; Ocean Drilling Program; ODP; Smectite (Area, 17Å); X-ray diffraction TEXTUR, clay fraction
    Materialart: Dataset
    Format: text/tab-separated-values, 1043 data points
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    facet.materialart.
    Unbekannt
    PANGAEA
    In:  Supplement to: Ehrmann, Werner; Grobe, Hannes; Fütterer, Dieter K (1991): Late Miocene to Holocene glacial history of east Antarctica revealed by sediments from sites 745 and 746. In: Barron, J; Larsen, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 119, 239-260, https://doi.org/10.2973/odp.proc.sr.119.208.1991
    Publikationsdatum: 2024-01-09
    Beschreibung: The sediments recovered at ODP Sites 745 and 746 in the Australian-Antarctic Basin are characterized by cyclic facies changes between clayey diatom oozes and diatomaceous clays ranging in age from late Miocene (about 10 Ma) to Quaternary. The gravel and terrigenous sand content of the sediments is used as an indicator of the intensity of ice rafting through time. Maxima are recorded at 8.7-7.9, 6.6-6.0, 5.0-4.4, and 4.0-3.2 Ma. The maxima in more recent times are much less pronounced and occur at 2.4-1.6 and 1.4-1.0 Ma. All sand- and gravel-sized terrigenous sediment particles are of gneissic or granitic origin and originated from the East Antarctic continent. The maxima of ice rafting recorded at Sites 745 and 746 do not appear to represent local phenomena. Rather they document major advances and decays of the Antarctic ice shelves and glaciers and therefore represent events of great importance for the reconstruction of the paleoceanography of the Southern Ocean and the glacial history of Antarctica. In general, ice rafting was pronounced in the late Miocene and early Pliocene epochs, which are characterized by repeated ice advances and retreats. Ice rafting was less intensive during the late Pliocene to Quaternary time period, when ice shelves remained relative stable. The clay minerals indicate the fluctuating influence of different source areas on the delivery of fine-grained terrigenous sediment components. Part of this material may have been delivered from the Permian Amery Formation or from equivalents of this formation.
    Schlagwort(e): 119-745B; 119-746A; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg119; Ocean Drilling Program; ODP
    Materialart: Dataset
    Format: application/zip, 10 datasets
    Standort Signatur Erwartet Verfügbarkeit
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