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《GEOLOGY OF ANHUI》 1994-Z1
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FANJINGSAN“KLIPPE”AND LANT1AN TECTONIC WINDOW──VIEWS ON THE NANGNAN一XUEFENG NAPPE

QiuYuanxi(Department of Geology, Zhongshan University)  
ResuIts of l:200,000 and I:50.000 scale regional geologial survey and large amounts of boreholedata support that the Fanjingshan “klippe”does not exist and the Nanming region , Southeastern Guizhou , is a synclinalbesin,not a tectonic window。Through field obeervation,the author holds that it is stiII Ilard to determine whether or notatectonic window exists in the tuntinn area.South Anhui,but it is certain that there are nappe structures in the Jiangnan一Xuefeng ancient land. They are parautochthonous nappes , with short displacement of less than 50km,which did notbring much change to the overall extension pattern of the regional sedimentary paleogeography and sedimentary facies inthe mar8inal area of Southeastern Yangtze landmass。 In the studicri area , distant nappes of Alpine type or Appalachiantype do not exist, and the Jiangnan一Xuefeng ancient land is not derived from the Cathaysia,Thrust or gravlty slidingstructures in the YangtZe landmass are of characteristics of intracontinental sutx1uction and in traplate compression or extension,quite different from the collision of two continents or plates。
【Fund】: 国家自然科学基金
【CateGory Index】: P54
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