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Authigenic Gypsum in Gas-Hydrate Associated Sediments from the East Coast of India (Bay of Bengal)

DRS at CSIR-National Institute of Oceanography

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Title Authigenic Gypsum in Gas-Hydrate Associated Sediments from the East Coast of India (Bay of Bengal)
 
Creator Kocherla, M.
 
Subject gypsum
authigenic minerals
gas hydrates
sediment analysis
 
Description Authigenic gypsum crystals, along with pyrite and carbonate mineralization, predominantly calcites were noticed in distinct intervals in a 32 m long piston core, collected in the gas hydrate-bearing sediments in the northern portion of the Krishna-Godavari basin, eastern continental margin of India at a water depth of 1691 m. X-ray diffraction and energy dispersive spectrum studies confirm presence of pyrite, gypsum, calcite, and other mineral aggregates. The occurrence of gypsum in such deep sea environment is intriguing, because gypsum is a classical evaporite mineral and is under saturated with respect to sea water. Sedimentological, geochemical evidences point to diagenetic formation of the gypsum due to oxidation of sulphide minerals (i.e. pyrite). Euhedral, transparent gypsum crystals, with pyrite inclusions are cemented with authigenic carbonates, possibly indicating that they were formed authigenically in situ in the gas hydrate-influenced environment due to late burial diagenesis involving sulphate reduction and anaerobic oxidation of methane (AOM). Therefore, the authigenic gypsums found in sediments of the Krishna-Godavari and Mahanadi offshore regions could be seen as one of the parameters to imply the presence of high methane flux possibly from gas hydrate at depth.
 
Date 2013-08-07T12:19:19Z
2013-08-07T12:19:19Z
2013
 
Type Journal Article
 
Identifier Acta Geologica Sinica, vol.87(3); 2013
no
http://drs.nio.org/drs/handle/2264/4342
 
Language en
 
Relation Acta_Geol_Sin_87.jpg
 
Rights An edited version of this paper was published by John Wiley/Geological Society of China. This paper is for R & D purpose.
 
Publisher Geological Society of China