MESOZOIC GRANITOIDS OF THE UPPER AMUR REGION: NEW SR, ND, AND O ISOTOPIC COMPOSITION DATA

dc.contributor.authorStrikha V.E.
dc.date.accessioned2024-11-09T08:38:21Z
dc.date.available2024-11-09T08:38:21Z
dc.date.issued2006
dc.description.abstractFirst data on the Sr, Nd, and O isotopic compositions in Mesozoic granitoids of the upper Amur region and previous data on the Sr and Nd isotopic compositions available for different-age granitoids are discussed. The upper Amur region comprises a spacious territory located between the Siberian and North China platforms. Based on literature data, the region includes the following major structural units: Aldan–Stanovoi, Baikal–Vitim, and Amur superterranes, Mongol–Okhotsk Foldbelt, and Umlekan–Ogodzha volcanoplutonic belt that unites and overlaps structures of the Amur Superterrane and the Mongol–Okhotsk Foldbelt.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13529065
dc.identifier.citationDoklady Earth Sciences, 2006, 409, 6, 944-947
dc.identifier.doi10.1134/S1028334X06060250
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46446
dc.subjectAmur superterrane
dc.titleMESOZOIC GRANITOIDS OF THE UPPER AMUR REGION: NEW SR, ND, AND O ISOTOPIC COMPOSITION DATA
dc.typeСтатья

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