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The Cenozoic deformation of the Alxa Block resulted directly from the evolution of the northern Qinghai-Tibetan Plateau. However, many data show that the deformation occurred only in the Middle-Late Miocene. Our studies show that the Altyn Tagh fault did not pass through the Alxa Block; on the contrary it went along the southern boundary of the Jintai-Huahai Basin, linking with the Helishan—southern...
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