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

Strikha V.E.

dc.contributor.author	Strikha V.E.
dc.date.accessioned	2024-11-09T08:38:21Z
dc.date.available	2024-11-09T08:38:21Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13529065
dc.identifier.citation	Doklady Earth Sciences, 2006, 409, 6, 944-947
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46446
dc.description.abstract	First 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.subject	Amur superterrane
dc.title	MESOZOIC GRANITOIDS OF THE UPPER AMUR REGION: NEW SR, ND, AND O ISOTOPIC COMPOSITION DATA
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06060250