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《GEOTECTONICA ET METALLOGENIA》 2000-01
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RECOGNITION OF ANCIENT TECTONIC RELATIVE LOCATION OF THE BIRU TERRAIN AND CUOQIN TERRAIN

LI Ben-liang1, XIA Bang-dong1, ZHANG Yong-jun2(1.Department of Earth Sciences,Nanjing University,Nanjing 210093, China)(2.Aero Geophysical Survey &Remote Sensing Center,Beijing 100083, China)  
Using the sandstone samples of C K formations in the Biru Terrain,Cuoqin Terrain and their peripheral areas,the authors make the tectonics property maps,QFL and QPLsLv of erosion areas,trace elements relationship map,Th Co Zr/10,common elements relationship map and K2O/Na2O SiO2 and by combination of field testing stone cross profile,analyze tectonic evolution.It indicates that before T3-J1 the Biru Terrain was located north of the Cuoqin Terrain.Then with the Bangonghu Nujiang suture(BNS)extending in J2 3,the Biru Terrain started to strike slip toward east.Up to J2 3 the Bangonghu Nujiang suture(BNS)had nearly closed,and the Biru Terrain fixed to its present location.According to the 1/ZTR factor the authors also deduced the approximate strike slip location,present E90°49′N31°34′,in J2 3.
【Fund】: 西南石油学院国家重点开放实验室和国家自然科学基金!(编号49972069)
【CateGory Index】: P547
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