中文摘要：

最近突然地西藏的高原和邻近的山高举发生在早更新世的结束。高原的 uplift 源于迟了的中生代 -- 新生代有压缩性的结构由于在亚洲大陆下面的印度板的 subduction。这个事件决定性地完成了盆山脉地势，新生代盆变丑，大规模干旱和西方的中国的 desertification 的形成。大洋洲的陨星影响事件发生了 ca。0.8 妈以前，在印度洋山脉的三角区域定位了(20

英文摘要：

The latest sharp uplift of the Tibetan Plateau and adjacent mountains occurred at the end of the early Pleistocene. The uplift of the Plateau resulted from Late Mesozoic-Cenozoic compressional structure due to the subduction of the Indian Plate beneath the Asian continent. This event definitively effected the formation of basin-mountain relief, Cenozoic basin deformation, large scale aridity and desertification of western China. The Australasian meteorites impact event happened ca. 0.8 Ma ago, located in the triangle area of the Indian Ocean ridge （20°S/67°E）. The impact may have resulted in an acceleration of speeding of the Indian Ocean ridge pushing the Indian Plate to subduct rapidly northward. Thus, the impact event can give reasonable explanation for the dynamic background of the latest rapid uplift of the Tibetan Plateau and the continental deformation of western China and even of the Middle Asia.