From the Cretaceous to the Early Cenozoic, it was uplifted again, until the Quaternary to build huge mountains with two large sedimentary basins on both sides.
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从白垩纪到早新生代,它再度隆升,直至第四纪时形成雄伟的高大山系,两侧形成相应的大型沈积盆地。
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