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

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dc.contributor.authorAshchepkov I.V.
dc.contributor.authorGerasimov P.A.
dc.contributor.authorKhmel'nikova O.S.
dc.contributor.authorAnoshin G.N.
dc.contributor.authorVladykin N.V.
dc.contributor.authorSaprykin A.I.
dc.date.accessioned2021-02-26T12:25:35Z
dc.date.available2021-02-26T12:25:35Z
dc.date.issued2001
dc.identifierhttps://elibrary.ru/item.asp?id=13386393
dc.identifier.citationDoklady Earth Sciences, 2001, 378, С. 4, 495-499
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25747
dc.titleTEMPERATURE 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.typeСтатья

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