GEOCHRONOLOGY AND CORRELATION OF MESOZOIC MAGMATIC COMPLEXES IN THE NORTHERN MARGIN OF THE AMURIAN SUPERTERRANE

dc.contributor.author	Sorokin A.A.
dc.contributor.author	Sorokin A.P.
dc.contributor.author	Ponomarchuk V.A.
dc.contributor.author	Kozyrev S.K.
dc.date.accessioned	2022-03-30T02:31:51Z
dc.date.available	2022-03-30T02:31:51Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13466713
dc.identifier.citation	Stratigraphy and Geological Correlation, 2004, 12, 6, 572-587
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36732
dc.description.abstract	A subject of discussion is age of rocks in Mesozoic volcano-plutonic belts of the epi-Paleozoic Amurian superterrane. Mesozoic volcanic and intrusive complexes of the northeastern Greater Khingan and western Umlekan-Ogodzha volcano-plutonic belts are dated using the 40Ar/39Ar method of isotopic geochronology. The results obtained and dates published before are used to elaborate the correlation scheme for magmatic rocks of both belts. Similarity and distinctions in Mesozoic evolution of two structural zones under consideration are elucidated for the Late Jurassic, Early Cretaceous, and Early-Late Cretaceous boundary periods.
dc.subject	Mesozoic
dc.title	GEOCHRONOLOGY AND CORRELATION OF MESOZOIC MAGMATIC COMPLEXES IN THE NORTHERN MARGIN OF THE AMURIAN SUPERTERRANE
dc.type	Статья
dc.subject.age	Mesozoic
dc.subject.age	Мезозой	ru

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