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New field and geophysical data about transpressional deformation: An improved model for the structural style of Sha Gou fault area in southern Ningxia, northeastern edge of Tibetan Plateau, China
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文摘

We studied the structural style near the northeastern edge of Tibetan Plateau.

The overall structural style is not characterized by large-scale thrust nappes.

A new transpressional shear model with significant strike-slip faulting is proposed.

This study concerns uplift of Tibetan Plateau and tectonic escape north of Himalaya.

This study will also help to reveal the genesis of the Southwestern Liupan Shan Basin.

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