摘要 : The South Anyui Fold System was formed at the end of the Early Cretaceous at the site of a closed oceanic basin as a result of the collision of the Chukotka microcontinent with the structures of the active margin of the Siberian c... 展开
作者 | Sokolov~ S. D. Tuchkova~ M.~ I Ledneva~ G.~ V Luchitskaya~ M.~ V Ganelin~ A.~ V Vatrushkina~ E. V. Moiseev~ A.~ V |
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作者单位 | |
期刊名称 | 《Geotectonics》 |
页码/总页数 | 697-716 / 20 |
语种/中图分类号 | 英语 / P5 |
关键词 | tectonics geodynamics terranes ophiolites island arcs turbidites Paleozoic Mesozoic South Anyui Suture Northeast Asia |
DOI | 10.1134/S0016852121050083 |
馆藏号 | P-141 |