EARLY CRETACEOUS GEODYNAMICS OF THE TRANSBAIKAL REGION: PALEOMAGNETIC ASPECT

dc.contributor.author	Metelkin D.V.
dc.contributor.author	Gordienko I.V.
dc.contributor.author	Klimuk V.S.
dc.contributor.author	Zhao X.
dc.date.accessioned	2022-01-15T07:43:07Z
dc.date.available	2022-01-15T07:43:07Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13442049
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 9, 1221-1226
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34338
dc.description.abstract	In Baikal region, Mesozoic depressions are widely noted. Their formation was accompanied by active volcanism. So far, nature of the volcanism is not totally clear. In connection with this, paleomagnetic investigations of Chikoi-Khilokskaya depression have been performed, Chikoi-Khilokskaya depression is one of the largest Mesozoic structures of Baikal region. Active volcanic processes occurred in range since 122 till 113 million years. Paleomagnetic analysis has been performed with the use of equipment of Paleomagnetic Center of Siberian Division of Russian Academy of Sciences and of Paleomagnetic Laboratory of California University. Results of the investigations have led to determination of paleomagnetic pole.
dc.subject	Cretaceous
dc.title	EARLY CRETACEOUS GEODYNAMICS OF THE TRANSBAIKAL REGION: PALEOMAGNETIC ASPECT
dc.type	Статья
dc.subject.age	Mesozoic::Cretaceous
dc.subject.age	Мезозой::Меловая	ru

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