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000057650 0247_ $$2DOI$$a10.1007/BF02703024
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000057650 084__ $$2WoS$$aGeosciences, Multidisciplinary
000057650 084__ $$2WoS$$aMultidisciplinary Sciences
000057650 1001_ $$0P:(DE-HGF)0$$aBanerjee, S.$$b0
000057650 245__ $$aStratigraphy, sedimentology and bulk organic geochemistry of black shales from the Proterozoic Vindhyan Supergroup (central India)
000057650 260__ $$aBangalore$$bIndian Acad. of Sciences$$c2006
000057650 300__ $$a37 - 48
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000057650 440_0 $$017461$$aJournal of Earth System Science$$v115$$x0253-4126$$y1
000057650 500__ $$aRecord converted from VDB: 12.11.2012
000057650 520__ $$aFour organic-rich shale units of the Proterozoic Vindhyan sedimentary succession have been scanned to reveal their origin and hydrocarbon potential. The wavy-crinkly nature of the carbonaceous laminae is suggestive of a microbial mat origin of the shales. These shales are thus different from Phanerozoic black shales which typically exhibit planar laminae. The hydrocarbon potential of the black shale units has been evaluated by Rock-Eval pyrolysis. Total organic carbon content of many of the shales exceeds 1%. The mean T-max for the black shales translate to a vitrinite reflectance range of 2.05-2.40% Rm based on standard conversion techniques. These shales have reached the catagenetic stage near the beginning of anthracite formation.
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000057650 65320 $$2Author$$aproterozoic
000057650 65320 $$2Author$$ablack shales
000057650 65320 $$2Author$$amicrobial mat
000057650 65320 $$2Author$$akerogen
000057650 65320 $$2Author$$amaturation
000057650 65320 $$2Author$$acatagenesis
000057650 7001_ $$0P:(DE-Juel1)VDB45705$$aDutta, S.$$b1$$uFZJ
000057650 7001_ $$0P:(DE-HGF)0$$aPaikaray, S.$$b2
000057650 7001_ $$0P:(DE-Juel1)VDB1006$$aMann, U.$$b3$$uFZJ
000057650 773__ $$0PERI:(DE-600)2081712-5$$a10.1007/BF02703024$$gVol. 115, p. 37 - 48$$p37 - 48$$q115<37 - 48$$tJournal of earth system science$$v115$$x0253-4126$$y2006
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