Coarse ice-rafted debris in the bottom sediments of the Kara Sea.
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dc.contributor.author | Lisitzin, Alexander P | |
dc.contributor.author | Kharin, Gennady S | |
dc.contributor.author | Chernysheva, E A | |
dc.coverage.spatial | MEDIAN LATITUDE: 71.386000 * MEDIAN LONGITUDE: 57.502600 * SOUTH-BOUND LATITUDE: 70.135500 * WEST-BOUND LONGITUDE: 55.033700 * NORTH-BOUND LATITUDE: 72.636500 * EAST-BOUND LONGITUDE: 59.971500 * MINIMUM ELEVATION: -143.0 m * MAXIMUM ELEVATION: -87.0 m | |
dc.date.accessioned | 2019-11-24T07:53:09Z | |
dc.date.available | 2019-11-24T07:53:09Z | |
dc.date.issued | 2004-07-12 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.762973 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.762973 | |
dc.identifier.citation | Lisitzin, Alexander P; Kharin, Gennady S; Chernysheva, E A (2004): Coarse ice-rafted debris in the bottom sediments of the Kara Sea. Translated from Okeanologiya, 2004, 44(3), 440-456, Oceanology, 44(3), 412-427 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/7621 | |
dc.description.abstract | Composition and distribution.of ice-rafted coarse debris from the Kara Sea bottom were investigated. This material was obtained on 42 stations in Cruise 49 of R/V Dmitry Mendeleev by Sigsby trawls, box corers, grabs, and gravity corers. Existence of two main petrographic provinces is suggested: (1) West Kara and (2) East Kara. They differ in composition and sources of debris material. It is supposed that debris was transported mainly by floating ice. In Upper Pleistocene time rafting by glaciers and icebergs was also very possible. | |
dc.format | text/tab-separated-values, 50 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.rights | CC-BY-3.0: Creative Commons Attribution 3.0 Unported | |
dc.rights | Access constraints: unrestricted | |
dc.source | Supplement to: Lisitzin, Alexander P; Kharin, Gennady S; Chernysheva, E A (2004): Coarse ice-rafted debris in the bottom sediments of the Kara Sea. Translated from Okeanologiya, 2004, 44(3), 440-456, Oceanology, 44(3), 412-427 | |
dc.subject | Aluminium oxide | |
dc.subject | Archive of Ocean Data | |
dc.subject | ARCOD | |
dc.subject | Atomic absorption spectrometry (AAS) | |
dc.subject | Atomic emission spectroscopy (AES) | |
dc.subject | Barium | |
dc.subject | Caesium | |
dc.subject | Calcium, lithogen | |
dc.subject | Calcium oxide | |
dc.subject | Chromium | |
dc.subject | Cobalt | |
dc.subject | DM49 | |
dc.subject | DM49-4376-5 | |
dc.subject | DM49-4380-1 | |
dc.subject | Dmitry Mendeleev | |
dc.subject | Grab | |
dc.subject | GRAB | |
dc.subject | Iron oxide, Fe2O3 | |
dc.subject | Kara Sea | |
dc.subject | Loss of ignition analysis | |
dc.subject | Loss on ignition | |
dc.subject | Magnesium oxide | |
dc.subject | Manganese oxide | |
dc.subject | Nickel | |
dc.subject | Phosphorus oxide | |
dc.subject | Potassium oxide | |
dc.subject | Rock type | |
dc.subject | Rubidium | |
dc.subject | Sample code/label | |
dc.subject | Scandium | |
dc.subject | Silicon dioxide | |
dc.subject | Sodium oxide | |
dc.subject | SPASIBAIII | |
dc.subject | Strontium | |
dc.subject | Sum | |
dc.subject | Titanium dioxide | |
dc.subject | Vanadium | |
dc.subject | X-ray fluorescence (XRF) | |
dc.subject | Zirconium | |
dc.title | Coarse ice-rafted debris in the bottom sediments of the Kara Sea. | |
dc.title.alternative | (Table 2) Chemical composition of ice-rafted brecciated crystalline schist and biotite-garnet crystalline schist from the Kara Sea | |
dc.type | Dataset |
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