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《Geological Survey and Research》 2006-04
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Study and Comparision on the Terrance of Taohe River and Minjiang River in Minxian-Dangchang Area of the Western Qinling——Discussion on Geomorphological Respones of the SN Tectonic Zone in China

GUO Jin-jing1,HAN Wen-feng1?2,LIANG Shou-yun2,LI Xue-feng 1(1.Department of Civil Engineering,Tianjin Institute of Urban construction,Tianjin 300384,China;2.College of Civil Engineering,Lanzhou University,Lanzhou 730000,China)  
Minxian-Wudu area in the western Qinling is just located at the intersection of Qinling-Qilian-Kulun EW tectonic zone and Helan-Chuandian SN tectonic zone and the northeastern fringe of uplifted or uplifting Qinghai-Tibet Plateau,where is in the gravitational gradient zone and crust thickness steep gradient zone circling Qinghai-Tibet Plateau.Its geomorphological characteristics,in particular,its stream geomo-phological evolution,can provide the latest messages on the interaction of uplift of Qinghai-Tibet Plateau and activity of SN active tectonic zone.Based upon the comparision for terrances of Taohe River(TR) and Minjiang River(MR) in this area and analysis for regional geomorphology it is suggested that this two rivers had been a river before the late Pleistocene(about 0.03 Ma BP),called ancient Mingjiang River(AMR),and Lintan-Zhuoni-Minxian sector of the present TR was the upper reach of AMR,Muzhailing-Minxian sector of TR was one of tributary streams of AMR.The geologically historical relation-ship between the TR and MR above is interpreted as the result of the NNE strike divide ridge appearing 0.03 Ma BP,which cut the hydraulic relation between the TR and MR.The NNE strike divide ridge in this area is suggested to be the geomorphological response of thermo-tectonic activity of the Helan-Chuandian SN tectonic zone and the external diffusion and rapid uplift of Qinghai-Tibet Plateau.
【Fund】: 交通部西部交通建设科技项目“国道212公路(兰州-重庆)陇南段修筑技术研究”子课题一“滑坡、泥石流的成因、分布分类、判别和区划研究”(200231800036-1)
【CateGory Index】: P546
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