(Table 2) Chemical composition of ice-rafted brecciated crystalline schist and biotite-garnet crystalline schist from the Kara Sea ...

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)...

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Bibliographic Details
Main Authors: Lisitzin, Alexander P, Kharin, Gennady S, Chernysheva, E A
Format: Dataset
Language:English
Published: PANGAEA 2004
Subjects:
Event label
Latitude of event
Longitude of event
Elevation of event
Sample code/label
Rock type
Silicon dioxide
Titanium dioxide
Aluminium oxide
Iron oxide, Fe2O3
Manganese oxide
Magnesium oxide
Calcium oxide
Sodium oxide
Potassium oxide
Phosphorus pentoxide
Loss on ignition
Sum
Chromium
Nickel
Cobalt
Vanadium
Scandium
Zirconium
Barium
Strontium
Calcium, lithogen
Rubidium
Caesium
Grab
X-ray fluorescence XRF
Loss of ignition analysis
Calculated
Atomic absorption spectrometry AAS
Atomic emission spectroscopy AES
DM49
Dmitry Mendeleev
Archive of Ocean Data ARCOD
Kara Sea
Online Access:https://dx.doi.org/10.1594/pangaea.762973
https://doi.pangaea.de/10.1594/PANGAEA.762973
Description
Summary: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. ... : 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 ...

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