Lateral extrusion of the northern Tibetan Plateau interpreted from seismic images, potential field data, and structural analysis of the eastern Kunlun fault
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文摘
The block between the Elashan and Riyueshan faults extruded southward. The eastern Kunlun fault was offset from the Diebu-Bailongjiang fault as a result. The Ruo'ergai basin is a complex pull-apart basin. The Mianlue suture was seismically identified beneath the Western Qinling orogen. Duplicated Moho is evident beneath the West Qinling orogen and the Ruo'ergai basin.

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