NAPHTHIDES IN LOWER DEVONIAN BASALTS IN THE NORTH MINUSINSK DEPRESSION

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dc.contributor.author Serebrennikova O.V.
dc.contributor.author Turov Yu.P.
dc.contributor.author Filippova T.Yu.
dc.contributor.author Vasil'ev B.D.
dc.date.accessioned 2022-01-13T08:02:18Z
dc.date.available 2022-01-13T08:02:18Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=13427387
dc.identifier.citation Doklady Earth Sciences, 2003, 390, 4, 604-606
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/34245
dc.description.abstract Lower Devonian amygdaloidal basalts in the North Minusinsk Depression contain abundant inclusions of natural solid bitumens [1-3]. Liquid hydrocarbon fluids were found in Lower Devonian rocks on the left wall of the Sokhochul Ravine at the junction of Hercynian tectonic structures (southern blank of the North Minusinsk Depression) with Salairides of the Kuznetsk Alatau Mountains.
dc.subject Devonian
dc.title NAPHTHIDES IN LOWER DEVONIAN BASALTS IN THE NORTH MINUSINSK DEPRESSION
dc.type Статья
dc.subject.age Paleozoic::Devonian
dc.subject.age Палеозой::Девонская ru


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