ISOTOPIC AGE OF RHYOLITES FROM THE TRIASSIC TURA GROUP OF THE KUSHMURUN GRABEN, THE TURGAI DEPRESSION

dc.contributor.authorRublev A.G.
dc.contributor.authorProshin E.E.
dc.contributor.authorShergina Yu.P.
dc.contributor.authorBogomolov E.S.
dc.date.accessioned2021-02-16T10:54:52Z
dc.date.available2021-02-16T10:54:52Z
dc.date.issued2001
dc.description.abstractIsotopic dating showed that rhyolites of the Kushmurun graben are divisible into two groups different in age. One group is close to the Induan-Olenekian boundary in its chronostratigraphic position and has K-Ar and Rb-Sr age of 247 ± 3 Ma. The Rb-Sr isochron age for another group is 162 ± 7 Ma and thus corresponds to the Middle Jurassic. The results obtained suggest that the available stratigraphic subdivision of deposits in the Kushmurun graben should be revised. They also elucidate the isotopic age of the Induan-Olenekian boundary.
dc.identifierhttps://elibrary.ru/item.asp?id=13368121
dc.identifier.citationStratigraphy and Geological Correlation, 2001, 9, 1, 36-42
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25040
dc.subjectKushmurun graben
dc.subjectIsotopic dating
dc.subjectTriassic
dc.subjectJurassic
dc.subject.ageMesozoic::Jurassicen
dc.titleISOTOPIC AGE OF RHYOLITES FROM THE TRIASSIC TURA GROUP OF THE KUSHMURUN GRABEN, THE TURGAI DEPRESSION
dc.typeСтатья

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