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dc.contributor.authorKocherla, M.
dc.date.accessioned2013-08-07T12:19:19Z
dc.date.available2013-08-07T12:19:19Z
dc.date.issued2013
dc.identifier.citationActa Geologica Sinica, vol.87(3); 2013
dc.identifier.otherno
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/4342
dc.description.abstractAuthigenic 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.
dc.language.isoen
dc.publisherGeological Society of China
dc.relation.requiresActa_Geol_Sin_87.jpg
dc.rightsAn edited version of this paper was published by John Wiley/Geological Society of China. This paper is for R & D purpose.
dc.subjectgypsum
dc.subjectauthigenic minerals
dc.subjectgas hydrates
dc.subjectsediment analysis
dc.titleAuthigenic Gypsum in Gas-Hydrate Associated Sediments from the East Coast of India (Bay of Bengal)
dc.typeJournal Article


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