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Coupling and Formation Mechanism of Continental Intraplate Basin and Orogen——Examples from the Qinghai-Tibetan Plateau and Adjacent Basins
详细信息   
摘要
There are very close relationship between orogenic belts and sedimentary basins, which show some features including interdependence of their spatial structures, mutual compensation of their materials, interaction of their tectonics, and simultaneity of their tectonic evolutions. A unified formation mechanism of continental orogenic belts and sedimentary basins is presented in this paper.

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