LOSS OF CONCENTRATED ORGANIC MATTER BY ROCKS DURING CATAGENESIS: A FACTOR OF GEODYNAMIC DESTABILIZATION
| dc.contributor.author | Yusupova I.F. | |
| dc.contributor.author | Abukova L.A. | |
| dc.contributor.author | Abramova O.P. | |
| dc.date.accessioned | 2026-04-25T09:33:03Z | |
| dc.date.issued | 2007 | |
| dc.description.abstract | Rocks with concentrated organic matter can be exemplified by oil shales, where solid organic matter (OM) is one of the rock-forming components. Sapropel oil shales with OM content of 20% and higher are widespread in the Precambrian–Holocene sections and characterized by very large reserves. | |
| dc.identifier | https://elibrary.ru/item.asp?id=15292282 | |
| dc.identifier.citation | Doklady Earth Sciences, 2007, 414, 1, 507-510 | |
| dc.identifier.doi | 10.1134/S1028334X07040034 | |
| dc.identifier.issn | 1028-334X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/52640 | |
| dc.title | LOSS OF CONCENTRATED ORGANIC MATTER BY ROCKS DURING CATAGENESIS: A FACTOR OF GEODYNAMIC DESTABILIZATION | |
| dc.type | Статья |
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