Distribution and Accumulation Rate of Hg in the Upper Quaternary Sediments of the Derugin Basin, Sea of Okhotsk.

Astakhov, A. S., Wallmann, Klaus , Ivanov, M. V., Kolesov, G. M. and Sattarova, V. V. (2007) Distribution and Accumulation Rate of Hg in the Upper Quaternary Sediments of the Derugin Basin, Sea of Okhotsk. Geochemistry International, 45 (1). pp. 47-61. DOI 10.1134/S0016702907010041.

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Abstract

Results of the study of contents and accumulation rates of Fe, Mn, and a number of trace elements in Upper Quaternary sediments of the Deryugin Basin are presented. Maps of the average contents and accumulation rates of excess Fe, Mn, Zn, Ba, Ni, Pb, Cu, and Mo in sediments of the first oxygen isotope stage (OIS) have been plotted. Anomalous contents and accumulation rates are confined to peripheral zones of the Deryugin sedimentary basin and large fracture zones. Different mechanisms of the influence of fluid-dynamic processes on the rate of hydrogenic and biogenic accumulation of ore elements are assumed.

Document Type: Article
Keywords: Hg, upper Quaternary sediments, Derugin Basin, Sea of Okhotsk
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
Refereed: Yes
Open Access Journal?: No
Publisher: Pleiades
Projects: Future Ocean, COMEX
Date Deposited: 03 Dec 2008 16:51
Last Modified: 29 May 2018 10:24
URI: https://oceanrep.geomar.de/id/eprint/7985

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