Two phases of Cenozoic deformation in the Wudu Basin, West Qinling (Central China): Implications for outward expansion of the Tibetan Plateau

Journal of Asian Earth Sciences(2022)

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摘要
•Wudu Basin involved into two phases of deformation due to uplift of the Tibetan Plateau.•The early one was resulted from the NNE-SSW shortening during the Late Oligocene.•The late one is reflected by the N-S shortening structures formed at the end Miocene.
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关键词
Structural analysis,Fault slip vectors,Tibetan Plateau,West Qinling Orogenic Belts,Wudu Basin
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