(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
Description
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.
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Publication Details
Subfield
Renewable Energy, Sustainability and the Environment
Field
Energy
Domain
Physical Sciences
Confidence Score
61%
Source
Scholar Data Model
Keywords
Event labelLatitude of eventLongitude of eventElevation of eventSample code/labelRock typeSilicon dioxideTitanium dioxideAluminium oxideIron oxide, Fe2O3Manganese oxideMagnesium oxideCalcium oxideSodium oxidePotassium oxidePhosphorus pentoxideLoss on ignitionSumChromiumNickelCobaltVanadiumScandiumZirconiumBariumStrontiumCalcium, lithogenRubidiumCaesiumGrabX-ray fluorescence (XRF)Loss of ignition analysisCalculatedAtomic absorption spectrometry (AAS)Atomic emission spectroscopy (AES)DM49Dmitry MendeleevArchive of Ocean Data (ARCOD)