GENETIC ASPECTS OF THE FORMATION OF CARBONACEOUS SUBSTANCES IN THE MINUSA BASIN

Pisotsky B.I.; Gottikh R.P.; Vasil'ev B.D.; Zhuravlev D.Z.

dc.contributor.author	Pisotsky B.I.
dc.contributor.author	Gottikh R.P.
dc.contributor.author	Vasil'ev B.D.
dc.contributor.author	Zhuravlev D.Z.
dc.date.accessioned	2024-11-02T11:07:50Z
dc.date.available	2024-11-02T11:07:50Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13522746
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1272-1276
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46355
dc.description.abstract	The carbonaceous substances confined to both igneous and terrigenous rocks are widespread in the Minusa intermontane trough of the Altai–Sayan region. The characteristics of bitumen from this region obtained with methods traditional for petroleum geochemistry. The formation of high-carbonic and high-molecular compounds is related to the thermal destruction of the dispersed organic matter (OM) as a result of the large-scale emplacement of basaltic magma in the Early Devonian and the subsequent condensation of sublimates in relatively cold areas.
dc.subject	Minusa basin
dc.title	GENETIC ASPECTS OF THE FORMATION OF CARBONACEOUS SUBSTANCES IN THE MINUSA BASIN
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080253
dc.subject.age	Paleozoic::Devonian
dc.subject.age	Палеозой::Девонская