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Evolution of drainage systems and its developing trend in connection with tectonic uplift of Eastern Kunlun Mt.

机译:东昆仑山构造演化与排水系统的演变及其发展趋势。

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摘要

The Eastern Kunlun Mt. Had been subjected to uplift together with the Qinghai-Xizang (Tibet) Plateau before the Early Pleistocene, and yet the Mt. Did not protrude out of the Plateau surface. During that period lakes spread all over the studied region, with the drainage systems being all short rivers flowing into the lakes. At the end of the Early Pleistocene, intensive tectonic uplift led to the rising of the Eastern Kunlun Mt. And made the Mt.
机译:东昆仑山在早更新世之前与青藏高原一起经历了隆升,而在没有突出到高原表面。在此期间,湖泊遍布整个研究区域,排水系统是所有流入湖泊的短河。在更新世初期,强烈的构造隆升导致了东昆仑山的崛起。并取得了山。

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