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《Journal of Earth Sciences and Environment》 2006-01
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Storage and Moving of Ore-forming Fluid of Dingjiashan-Gulushan Gold Deposit

LIU Xin-hui~1,LIU Shuang~1,LI Yuan~1,WEI Kuan-yi~2 (1.5th Gold Geological Detachment,CAPF,Xin'an 710100,Shaanxi,China; 2.School of Earth Sciences and Resources Management,Chang'an University,Xi'an 710054, Shaanxi,China)  
The upper Devonian Nanyangshan Formation and lower Carboniferous Yuanjiagou Formation layers are the source rocks of the Jinlongshan-Qiuling gold mine. The source rocks are frequent interbedding of fine-grained clastic rocks and carbonate rocks.Fine-grained sandstones,siltstones and carbonate rocks are better than shales and slates in the sense of physical nature for ore-forming fluid.In the metallogenic course,fracturing deformations closely correspond to the formation,storage and moving of the ore-forming fluid.The process is: ① primary structures result in the first collection of the ore-forming fluid; ② the first fracturing deformation results in the collection of the ore-forming fluid;③ the second fracturing deformation results in the moving and gold deposition of the ore-forming fluid;④ the third fracturing deformation results in the further collection of the ore-forming fluid and the enrichment of the gold deposits;⑤ the fourth fracturing deformation corresponds to the quartz-calciate vein.
【Fund】: 国家经济贸易委员会项目(陕西镇安金龙山矿区及外围岩金普查(2001~2004))
【CateGory Index】: P618.51
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