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)
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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