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| Home > Publications database > Stratigraphy, sedimentology and bulk organic geochemistry of black shales from the Proterozoic Vindhyan Supergroup (central India) > print |
| Home > Publications database > Stratigraphy, sedimentology and bulk organic geochemistry of black shales from the Proterozoic Vindhyan Supergroup (central India) > print |
| 001 | 57650 | ||
| 005 | 20161225213213.0 | ||
| 024 | 7 | _ | |2 DOI |a 10.1007/BF02703024 |
| 024 | 7 | _ | |2 WOS |a WOS:000236375500004 |
| 037 | _ | _ | |a PreJuSER-57650 |
| 041 | _ | _ | |a eng |
| 082 | _ | _ | |a 000 |
| 084 | _ | _ | |2 WoS |a Geosciences, Multidisciplinary |
| 084 | _ | _ | |2 WoS |a Multidisciplinary Sciences |
| 100 | 1 | _ | |a Banerjee, S. |b 0 |0 P:(DE-HGF)0 |
| 245 | _ | _ | |a Stratigraphy, sedimentology and bulk organic geochemistry of black shales from the Proterozoic Vindhyan Supergroup (central India) |
| 260 | _ | _ | |a Bangalore |b Indian Acad. of Sciences |c 2006 |
| 300 | _ | _ | |a 37 - 48 |
| 336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
| 336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
| 336 | 7 | _ | |a article |2 DRIVER |
| 440 | _ | 0 | |a Journal of Earth System Science |x 0253-4126 |0 17461 |y 1 |v 115 |
| 500 | _ | _ | |a Record converted from VDB: 12.11.2012 |
| 520 | _ | _ | |a Four 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. |
| 536 | _ | _ | |a Geosysteme - Erde im Wandel |c P21 |2 G:(DE-HGF) |0 G:(DE-Juel1)FUEK405 |x 0 |
| 588 | _ | _ | |a Dataset connected to Web of Science |
| 650 | _ | 7 | |a J |2 WoSType |
| 653 | 2 | 0 | |2 Author |a proterozoic |
| 653 | 2 | 0 | |2 Author |a black shales |
| 653 | 2 | 0 | |2 Author |a microbial mat |
| 653 | 2 | 0 | |2 Author |a kerogen |
| 653 | 2 | 0 | |2 Author |a maturation |
| 653 | 2 | 0 | |2 Author |a catagenesis |
| 700 | 1 | _ | |a Dutta, S. |b 1 |u FZJ |0 P:(DE-Juel1)VDB45705 |
| 700 | 1 | _ | |a Paikaray, S. |b 2 |0 P:(DE-HGF)0 |
| 700 | 1 | _ | |a Mann, U. |b 3 |u FZJ |0 P:(DE-Juel1)VDB1006 |
| 773 | _ | _ | |a 10.1007/BF02703024 |g Vol. 115, p. 37 - 48 |p 37 - 48 |q 115<37 - 48 |0 PERI:(DE-600)2081712-5 |t Journal of earth system science |v 115 |y 2006 |x 0253-4126 |
| 909 | C | O | |o oai:juser.fz-juelich.de:57650 |p VDB |
| 913 | 1 | _ | |k P21 |v Geosysteme - Erde im Wandel |l Geosysteme - Erde im Wandel |b Umwelt |0 G:(DE-Juel1)FUEK405 |x 0 |
| 914 | 1 | _ | |a Nachtrag |y 2006 |
| 915 | _ | _ | |0 StatID:(DE-HGF)0010 |a JCR/ISI refereed |
| 920 | 1 | _ | |k ICG-V |l Sedimentäre Systeme |d 31.12.2006 |g ICG |0 I:(DE-Juel1)VDB51 |x 1 |
| 970 | _ | _ | |a VDB:(DE-Juel1)90682 |
| 980 | _ | _ | |a VDB |
| 980 | _ | _ | |a ConvertedRecord |
| 980 | _ | _ | |a journal |
| 980 | _ | _ | |a I:(DE-Juel1)ICG-5-20090406 |
| 980 | _ | _ | |a UNRESTRICTED |
| 981 | _ | _ | |a I:(DE-Juel1)ICG-5-20090406 |
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