(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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Metrics

Dataset Index

0.3

FAIR Score

94%

Citations

0

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

PANGAEA

License

Creative Commons Attribution 3.0 Unported

Assigned Domain

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)

Normalization Factors

FT

94.23

CTw

1.00

MTw

1.00