Mineral composition of sedimentary matter in the Caspian Sea
- Authors: Lukashin V.N.1, Lisitzin A.P.1, Dara O.M.1, Kozina N.V.1, Klyuvitkin A.A.1, Novigatsky A.N.1
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Affiliations:
- Shirshov Institute of Oceanology
- Issue: Vol 56, No 6 (2016)
- Pages: 852-862
- Section: Marine Geology
- URL: https://journals.rcsi.science/0001-4370/article/view/149309
- DOI: https://doi.org/10.1134/S0001437016060096
- ID: 149309
Cite item
Abstract
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.
About the authors
V. N. Lukashin
Shirshov Institute of Oceanology
Author for correspondence.
Email: lukashin@ocean.ru
Russian Federation, Moscow
A. P. Lisitzin
Shirshov Institute of Oceanology
Email: lukashin@ocean.ru
Russian Federation, Moscow
O. M. Dara
Shirshov Institute of Oceanology
Email: lukashin@ocean.ru
Russian Federation, Moscow
N. V. Kozina
Shirshov Institute of Oceanology
Email: lukashin@ocean.ru
Russian Federation, Moscow
A. A. Klyuvitkin
Shirshov Institute of Oceanology
Email: lukashin@ocean.ru
Russian Federation, Moscow
A. N. Novigatsky
Shirshov Institute of Oceanology
Email: lukashin@ocean.ru
Russian Federation, Moscow
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