Инд. авторы:	Kruk N.N., Golozubov V.V., Bayanova T.B., Kasatkin S.A.
Заглавие:	Composition, age, and tectonic position of granitoids of the Shmakovka complex
Библ. ссылка:	Kruk N.N., Golozubov V.V., Bayanova T.B., Kasatkin S.A. Composition, age, and tectonic position of granitoids of the Shmakovka complex // Russian Journal of Pacific Geology. - 2016. - Vol.10. - Iss. 2. - P.132-140. - ISSN 1819-7140. - EISSN 1819-7159.
Внешние системы:	DOI: 10.1134/S1819714016020056; SCOPUS: 2-s2.0-84969974924; WoS: 000376273800004;
Реферат:	eng: The geological, geochemical, and geochronological data on the granitiods of the Shmakovka massif, which represents a petrotype of the synonymous complex (southern Russian Primorye), show that the granitoid intrusions of the Shmakovka Complex play a “coupling” role, occurring in different blocks of the Khanka composite terrane. The geochemical and isotopic features of the granitoids indicate that their formation resulted from melting of a “mixed,” substantially metapelite, source similar to the most intensely metamorphosed rocks of the Khanka massif. According to U–Pb measurements, the granitoids are 490 ± 1 Ma old. The analysis of the distribution of Early Paleozoic I-, S-, and A-type granitoids in southern Primorye reveals that Late Cambrian–Early Ordovician endogenic events marked the amalgamation of Precambrian–Early Paleozoic blocks and the eventual formation of the Bureya–Jiamusi superterrane (Bureya–Khanka orogenic belt). © 2016, Pleiades Publishing, Ltd.
Ключевые слова:	southern Primorye; Russia; Khanka massif; granitoids; geochronology; geochemistry; Bureya–Jiamusi superterrane;
Издано:	2016
Физ. характеристика:	с.132-140