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《Acta Sedimentologica Sinica》 2001-01
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On Implications of the Devonian Hydrothermal Sedimentary Facies in the Qinling Orogeny

FANG Wei xuan 1,3 ZHANG Guo wei 2 HU Rui zhong 1 LIU Fang jie 3 1(LODG Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002) 2(Northwest University, Department of Geology, Xi'an 710069) 3(Northwest Geological Exploratio  
The Qinling orogenic belt is located in the central China and is one of the most important intracontinental orogeny in the world. Devonian sedimentary basins are the major accumulation structures for Au Ag Pb Zn deposits in the area. Fengtai Devonian pull apart basin, one of the accumulation basins in the Qinling orogeny, hosted a series of large superlarge Au Pb Zn deposits such as Qiandongshan and Dongtangzi large Pb Zn deposits and Baguamiao superlarge Au deposits. Lead zinc orebodies hosted at a suite of hydrothermal depositional rocks in the three order hydrothermal basins. Therefore, research on relationship between the hydrothermal depositional facies and the three order hydrothermal basin is the best way to understand the relationship between metal deposits and the hydrothermal depositional basin. The concept of hydrothermal sedimentary rock facies at the Devonian in the Qinling orogeny has been initiated. Relationships between tectonic hydrothermal sedimentary facies and paleo geographic framework of sedimentary basin, between hydrothermal sedimentary facies and mineralization of hydrothermal depositions, and between hydrothermal sedimentary facies and tectonic geographic framework are very important in the analysis of sedimentary basin. On the basis of associations of the hydrothermal sedimentary facies, sedimentary lithofacies, and sedimentary system, the Qiandongshan Shuangshipu third order hydrothermal depositional basin has been analyzed in this paper. Three depositional systems are recognized in the Qiandongshan Shuangshipu third order hydrothermal depositional basin. Carbonate rock formation was formed in a shallow water environment at the beginning of the three order basin while fine clastic rock formation was formed in a shallow water environment at the closedown of the three order basin. The hydrothermal depositional system between them was developed in half deep or deep water, limited, reducing environment in the three order hydrothermal basin. NE trending synfault were responsible for the formation of the Qiandongshan Shuangshipu downfaulted three order basin. Based on analysis of paleotectonics and basin filling sediments, the data suggests that the Qiandongshan Shuangshipu three order basin with hydrothermal depositions were probably formed in tectonics field of tensile shear stress in the Middle Late Devonian.
【Fund】: 国家重大基础研究规划项目 !(G1 9990 4 32 0 0 );; 国家自然科学基金秦岭重点项目! (批准号 :49732 0 80 );; 中国有色金属工业总公司人
【CateGory Index】: P588.2
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