Mineral composition of sedimentary matter in the Caspian Sea


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详细

Data on the mineral composition of sedimentary matter and its fluxes in the sediment system of the Caspian Sea are presented. River runoff, aerosols, particulate matter from sediment traps, and the upper layer (0–1 cm) of bottom sediments are considered. The contents of detrital minerals (quartz, albite, and K-feldspar), clay minerals (illite, chlorite, and kaolinite), and carbonates (calcite, Mg-calcite, dolomite, aragonite, and rhodochrosite) are determined. Gypsum was found in bottom sediments but is absent in the other object of the sediment system.

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V. Lukashin

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: lukashin@ocean.ru
俄罗斯联邦, Moscow

A. Lisitzin

Shirshov Institute of Oceanology

Email: lukashin@ocean.ru
俄罗斯联邦, Moscow

O. Dara

Shirshov Institute of Oceanology

Email: lukashin@ocean.ru
俄罗斯联邦, Moscow

N. Kozina

Shirshov Institute of Oceanology

Email: lukashin@ocean.ru
俄罗斯联邦, Moscow

A. Klyuvitkin

Shirshov Institute of Oceanology

Email: lukashin@ocean.ru
俄罗斯联邦, Moscow

A. Novigatsky

Shirshov Institute of Oceanology

Email: lukashin@ocean.ru
俄罗斯联邦, Moscow

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