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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