(Table 2) Chemical composition of ice-rafted brecciated crystalline schist and biotite-garnet crystalline schist from the Kara Sea
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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2004
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| _version_ | 1867169982590222336 |
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| author | Lisitzin, Alexander P Kharin, Gennady S Chernysheva, E A |
| author_facet | Lisitzin, Alexander P Kharin, Gennady S Chernysheva, E A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_762973 |
| institution | PANGAEA |
| language | en |
| publishDate | 2004 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 2) Chemical composition of ice-rafted brecciated crystalline schist and biotite-garnet crystalline schist from the Kara Sea Lisitzin, Alexander P Kharin, Gennady S Chernysheva, E A Aluminium oxide; Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Atomic emission spectroscopy (AES); Barium; Caesium; Calcium, lithogen; Calcium oxide; Calculated; Chromium; Cobalt; DM49; DM49-4376-5; DM49-4380-1; Dmitry Mendeleev; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Kara Sea; Latitude of event; Longitude of event; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium oxide; Rock type; Rubidium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; SPASIBAIII; Strontium; Sum; Titanium dioxide; Vanadium; X-ray fluorescence (XRF); Zirconium 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. |
| title | (Table 2) Chemical composition of ice-rafted brecciated crystalline schist and biotite-garnet crystalline schist from the Kara Sea |
| topic | Aluminium oxide; Archive of Ocean Data; ARCOD; Atomic absorption spectrometry (AAS); Atomic emission spectroscopy (AES); Barium; Caesium; Calcium, lithogen; Calcium oxide; Calculated; Chromium; Cobalt; DM49; DM49-4376-5; DM49-4380-1; Dmitry Mendeleev; Elevation of event; Event label; Grab; GRAB; Iron oxide, Fe2O3; Kara Sea; Latitude of event; Longitude of event; Loss of ignition analysis; Loss on ignition; Magnesium oxide; Manganese oxide; Nickel; Phosphorus pentoxide; Potassium oxide; Rock type; Rubidium; Sample code/label; Scandium; Silicon dioxide; Sodium oxide; SPASIBAIII; Strontium; Sum; Titanium dioxide; Vanadium; X-ray fluorescence (XRF); Zirconium |
| url | https://doi.org/10.1594/PANGAEA.762973 |