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Petrography, diagenesis and depositional environment of the Late Proterozoic cave-temple arenites of Badami Group, Karnataka

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dc.contributor.author Mahender, K.
dc.contributor.author Fernandes, B.
dc.date.accessioned 2015-06-03T08:09:01Z
dc.date.available 2015-06-03T08:09:01Z
dc.date.issued 2002
dc.identifier.citation Recent Researches on the Proterozoic Basins of India, Ed. by: R. Guhey, P. Thakur, R. Sridhar Rao. Govt. Science College, Raipur. 2002; 17-25. en_US
dc.identifier.uri http://irgu.unigoa.ac.in/drs/handle/unigoa/1503
dc.description.abstract The Late Proterozoic Cave-Temple Arenite member of Badami Group comprising predominantly of sandstone forms one of the most interesting litho-units exposed around Badami for its prominent topographic expression (flat topped barren hillocks) along with a host of sedimentary structures viz. Cross-bedding, ripple marks, groove casts, convolute lamination etc. These sandstones are medium to coarse grained, moderate well sorted, subrounded to well rounded and belong to the quartz arenite to sub-arkose categories. Compositionally these rocks show considerabie maturity with abundant quartz (78-96 percent) and subordinate feldspars having undergone both the physical (compaction and pressure solution) and chemical (silica, calcite and hematite cementation) diagenetic changes. Mineralogical composition of these sandstones indicates a principal recycled orogen source. The variety of sedimentary structures and the textural characters suggest a shallow marine depositional environment of the sandstones.
dc.subject Earth Science en_US
dc.title Petrography, diagenesis and depositional environment of the Late Proterozoic cave-temple arenites of Badami Group, Karnataka en_US
dc.type Conference article en_US


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