GRANODIORITES OF THE GRENVILLE PHASE IN THE KOKCHETAV BLOCK, NORTHERN KAZAKHSTAN

dc.contributor.authorLetnikov F.A.
dc.contributor.authorKotov A.B.
dc.contributor.authorSal'Nikova E.B.
dc.contributor.authorRizvanova N.G.
dc.contributor.authorMakeev A.F.
dc.contributor.authorShershakova M.M.
dc.contributor.authorShershakov A.V.
dc.date.accessioned2026-05-03T08:16:04Z
dc.date.issued2007
dc.description.abstractThe Kokchetav Block is composed of Precambrian metamorphic rocks of the Zerenda and Sharyk groups. The Zerenda Group (amphibolite-facies rocks) is overlain with geological and metamorphic unconformities by greenschists of the Sharyk Group. Based on the U–Pb zircon dating, gneisses of the Zerenda Group in the central Kokchetav Block are estimated at 1300–1900 Ma.
dc.identifierhttps://elibrary.ru/item.asp?id=15292488
dc.identifier.citationDoklady Earth Sciences, 2007, 417, 1, 1195-1197
dc.identifier.doi10.1134/S1028334X07080132
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/52823
dc.subject.agePrecambrian::Proterozoic::Mesoproterozoic
dc.subject.ageДокембрий::Протерозой::Мезопротерозойская
dc.titleGRANODIORITES OF THE GRENVILLE PHASE IN THE KOKCHETAV BLOCK, NORTHERN KAZAKHSTAN
dc.typeСтатья

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