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《Geotectonica Et Metallogenia》 2009-02
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Geological Features and Ore-Controlling Factors of the Yangshan Gold Field in Wen County,Gansu Province

GUO Junhua1,MAO Shidong1,2,3,CHEN Yanjing2,4,QIN Yan2,YANG Fuli1,LI Jianzhong1 and NAN Zhenglu1(1.The 12th Detachment of Gold Headquarters of China Armed Police Force,Chengdu 610036,Sichuan,China;2.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,Guangdong,China;3.Graduate School of the Chinese Academy of Sciences,Beijing 100049,China;4.Key Laboratory of Orogen and Crust Evolution,Peking University,Beijing 100871,China)  
The Yangshan gold-field,Wen County,Gansu Province,is the largest gold system in China.It has been recently discovered near the Mian-Lue geosuture zone in the western Qinling Orogen.As a Carlin-like gold-system,the deposit is located in the Wenxian arc-shaped tectonic zone and hosted in the Sanhekou Group of Devonian.Statistics of data from drillings and tunnels in the Anba exploration district of the Yangshan gold-field shows that all the orebodies are controlled by the Anchanghe-Guanyinba fault system comprising of the backbones and subsidiary brittle-ductile shear zones or fractures.The majority of orebodies locate in fractured pelitic and silty phyllites,with a minority in the pre-ore Indosinian granite-porphyry dykes or their contact zones,suggesting that the Indosinian granite magmatism was not,as interpreted in previous studies,the dominant factor to cause gold mineralization.Combining with regional geological study,we argue that the Sanhekou Group and its underlying strata such as the Bikou Group provided ore-fluids and metallogenic materials for the Yangshan gold-system during the Early Jurassic orogenesis,while the pelitic and silty phyllites of the Sanhekou Group provided favorable loci for ore-fluid accumulation and ore-metal discharge.The pre-ore granite-porphyry dykes emplaced along the Anchanghe-Guanyinba fault-system.Despite of their paucity,they could also focus and trap ore-fluids,and host gold orebodies.Moreover,due to great difference in strength between the phyllites and the porphyry dykes,most of the porphyry dyke-phyllite contact zones became brittle-ductile shear zones during collisional orogenesis and favorably accommodated ore-fluid circulating,focusing and gold mineralization.
【Fund】: 国家973项目(编号2006CB403508);; 国家自然科学基金项目(编号40425006和40703010);; 中国科学院百人计划项目和武警黄金部队科研项目联合资助
【CateGory Index】: P618.51
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