PREDICTION OF THE DIAMOND POTENTIAL OF TRIASSIC ROCKS IN TAIMYR

dc.contributor.authorGrakhanov S.A.
dc.contributor.authorYadrenkin A.V.
dc.date.accessioned2026-04-25T09:32:56Z
dc.date.issued2007
dc.description.abstractThe diamond potential of Taimyr was first predicted by V.S. Sobolev and G.G. Moor after study of samples of micaceous kimberlites discovered by N.N. Urvantsev in 1929. Alkaline basic rocks, similar to the kimberlite-associated melilitic basalts of South Africa, were discovered in Taimyr by Sobolev [1] and Moor (based on consultations with Sobolev) [14]. Sobolev made recommendations pertaining to the prospecting for kimberlites and diamonds in a special report submitted to Classified Report Funds of the Karpinskii All-Russia Research Institute of Geology, St. Petersburg in 1941 (inventory no. 1773).
dc.identifierhttps://elibrary.ru/item.asp?id=15292221
dc.identifier.citationDoklady Earth Sciences, 2007, 417, 1, 1147-1150
dc.identifier.doi10.1134/S1028334X07080028
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/52618
dc.subjectTriassic
dc.subject.ageMesozoic::Triassic
dc.subject.ageМезозой::Триасовая
dc.titlePREDICTION OF THE DIAMOND POTENTIAL OF TRIASSIC ROCKS IN TAIMYR
dc.typeСтатья

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