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《Petroleum Geology & Oilfield Development in Daqing》 2005-02
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Geochemical characteristics and their tectonic implications of early Yanshan granitoid in Shuanghu area of Qiangtang basin of Tibet

LI Yan-ping~(1, 2), LIN Zhen-hong~1, ZHENG Jian-bin~1,YI San-quan~2,TENG Yu-hong~2, WANG Xiu-yan~2 (1.College of Marine Geosciences,Ocean University of China, Qingdao 266003,China;2.Branch of Daqing Petroleum Institute, Qinhuangdao 066004,China)  
Amugang early Yanshan granitoid in Shuanghu area of Tibet Qiangtang basin crop out in the eastern central uplift zone of Qiangtang basin. On the basis of geochemical characteristics and tectonic setting discrimination diagrams,Amugang early Yanshan granitoid are described as strongly peraluminous (SP) granite with S type in large volumes and ACGI type in small volumes;the former granite are similar to Tibet Gabug ones in trace element and REE formed in tectonic setting of syn-collision;the later granite is generated in tectonic setting of CAG and IAG.But on account of these granitoid all formed after the climax of main collision suture,folding,deforming and high-pressure regional metamorphic event,ACGI type granite associated with SP granite might generated in the same tectonic setting-post-collision,Amugang early Yanshan granitoid is thought to be formed in tectonic setting of post-collision.
【CateGory Index】: P588.121
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