TEMPERATURE GRADIENT AND STRUCTURE OF THE LITHOSPHERIC BLOCK BENEATH THE SOUTHEASTERN MARGIN OF THE SIBERIAN CRATON: DISINTEGRATED XENOLITH EVIDENCE FROM KIMBERLITIC PIPES OF THE ALDAN SHIELD

dc.contributor.author	Ashchepkov I.V.
dc.contributor.author	Gerasimov P.A.
dc.contributor.author	Khmel'nikova O.S.
dc.contributor.author	Anoshin G.N.
dc.contributor.author	Vladykin N.V.
dc.contributor.author	Saprykin A.I.
dc.date.accessioned	2021-02-26T12:25:35Z
dc.date.available	2021-02-26T12:25:35Z
dc.date.issued	2001
dc.identifier	https://elibrary.ru/item.asp?id=13386393
dc.identifier.citation	Doklady Earth Sciences, 2001, 378, С. 4, 495-499
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/25747
dc.title	TEMPERATURE GRADIENT AND STRUCTURE OF THE LITHOSPHERIC BLOCK BENEATH THE SOUTHEASTERN MARGIN OF THE SIBERIAN CRATON: DISINTEGRATED XENOLITH EVIDENCE FROM KIMBERLITIC PIPES OF THE ALDAN SHIELD
dc.type	Статья

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