DEGREE OF THERMAL IMPACT ON THE PERIPHERY OF THE SIBERIAN CRATON IN THE PHANEROZOIC

dc.contributor.author	Letnikov F.A.
dc.contributor.author	Krasil'nikova E.E.
dc.contributor.author	Kostitsyn Yu.A.
dc.contributor.author	Mishina E.I.
dc.date.accessioned	2024-11-02T11:07:38Z
dc.date.available	2024-11-02T11:07:38Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520510
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 5, 706-708
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46314
dc.description.abstract	The crystalline basement of the Siberian Craton is exposed as fragments in the Sharyzhalgai inlier, which is separated by the Main Sayan fault from Paleozoic rocks of the Slyudyanka crystalline complex and is bounded by the ~70-km-long Baikal coastline from the Settlement of Kultuk to port of Lake Baikal. The geological boundary between Sharyzhalgai and surrounding Caledonides is at the Lake Baikal floor. The spatial association of Archean and Proterozoic rocks with Paleozoides has repeatedly inspired researchers to search for traces of endogenous influence of the Paleozoic framing on the rocks and basement of the platform.
dc.subject	Siberian craton
dc.title	DEGREE OF THERMAL IMPACT ON THE PERIPHERY OF THE SIBERIAN CRATON IN THE PHANEROZOIC
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06050059

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