Origin of the Elikanskii granite–gneiss swell in the West Stanovoi terrane of the Central Asian Fold Belt: Results of structural studies

被引：0
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作者：
A. M. Mazukabzov
A. B. Kotov
T. M. Skovitina
E. V. Sklyarov
A. M. Larin
机构：
[1] Russian Academy of Sciences,Institute of the Earth’s Crust, Siberian Branch
[2] Russian Academy of Sciences,Institute of Precambrian Geology and Geochronology
[3] Far East Federal University,undefined
来源：
Doklady Earth Sciences | 2016年 / 467卷
关键词：
Breccia; DOKLADY Earth Science; Argun; Detachment Zone; Central Asian Fold Belt;
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摘要：
Structural studies showed that the Elikanskii granite–gneiss swell is similar to the Late Mesozoic Cordilleran-type metamorphic core complexes distinguished in the southern part of the Eravninskii terrane and in the northeastern part of the Argun–Idermeg superterrane of this belt.
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页码：224 / 227
页数：3
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