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《Remote Sensing for Land & Resources》 2010-S1
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Eastward Migration of the Watershed of Inflow and Outflow Rives in the Mid-southern Qinghai-Tibet Plateau and the "Nagqu Movement"

SUN Yan-gui,ZHANG Kun,YU Jing-hui,MA Shi-bin(Institute of Geological Survey of Qinghai Province,Xining 810012,China)  
Making use of the remote sensing technique and field survey,the authors have studied the Quaternary geology of the Qinghai-Tibet Plateau since 2003,and the results indicate that the watershed of China's inflow rivers and outflow rivers in the mid-southern Qinghai-Tibet Plateau was formed in early Holocene.The Nagqu Movement that occurred at the last stage of late Pleistocene was an important crust movement forming the dividing range.The remote sensing survey also discovered that the dividing range was situated in the Tangra Yumco area.The crust movement resulted in eastward migration of the watershed for 500 km,and the early riverhead area of the Nujiang River consisting of the Siling Co and Namo Co lakes became inland basins.Based on the results of the remote sensing survey of the Quaternary geology which mainly include the fossil river courses,the angular unconformity between Pleistocene and Holocene and the Nagqu movement in the mid-southern Qinghai-Tibet Plateau,this paper deals systematically with these phenomena and regularities.
【CateGory Index】: P627;P534.63
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