ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西藏尕尔穷—嘎拉勒铜金矿集区成矿规律、矿床模型与找矿方向
  
关键词:Ga’erqiong-Galale ore field  metallogensis  deposit model  porphyry-skarn ore body  Bangong Co-Nujiang River metallogenic belt
基金项目:国家自然科学基金项目(编号: 41172077);国家973项目(编号: 2011CB403103);国土资源部公益性行业科研专项项目(编号: 201011013-3)
作者单位E-mail
唐菊兴 中国地质科学院矿产资源研究所 tangjuxing@126.com 
张志 成都理工大学  
李志军 成都理工大学  
孙燕 成都理工大学  
姚晓峰 中国地质大学(北京)  
胡正华 江西省地质调查研究院  
王红星 成都理工大学  
宋俊龙 成都理工大学  
何林 西藏自治区地质矿产勘查开发局第二地质大队  
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摘要:
The Metallogensis, Deposit Model and Prospecting Direction of the Ga’erqiong-Galale Copper-gold Ore Field, Tibet
      Located in the south of western Bangong Co-Nujang River metallogenic belt of north Gangdise, the Ga’erqiong-Galale copper-gold ore field possesses lots of ore body types (porphyry type, skarn type and iron oxide-copper-gold type) and high gold grade (up to 205 g/t) and unique structural position, thus having great research significance. According to systematic summary of ore concentration areas and systematic analysis of data, the authors identified ore characteristics, found a large number of native gold and intermetallic compounds, and summarized the metallogensis. It is considered that metallization was mainly associated with emplacement of quartz diorite and granodiorite in the late phase of Yanshanian period, the evolution time between diagenesis and mineralization was about 1 Ma, and the mineralization in the area was characterized by the vertical zoning of copper-gold in the upper part and molybdenum in the lower part. S, Pb isotopes suggest that the metallogenic material had characteristics of crust-mantle mixing. During the emplacement and fractionation evolution of metaluminous-weak peraluminous calc-alkaline-high-K calc-alkaline magmatite, the porphyry-skarn type copper-gold-molybdenum ore bodies were formed in the area of pluton uplifting and along the contact zone between the pluton and the Cretaceous carbonate, whereas iron oxide-copper-gold type ore bodies were formed at the edge of pluton’s tectonic fracture zone (F1 fault). On such a basis, the authors have established the porphyry-skarn-iron oxide-copper-gold type “three-position” mineralization deposit model of magmatite- strata-ore-controlling structure. Based on these data, the authors indicate the prospecting direction in search for new ore bodies in the ore field.
TANG Ju-xing,ZHANG Zhi,LI Zhi-jun,SUN Yan,YAO Xiao-feng,HU Zheng-hua,WANG Hong-xing,SONG Jun-long,HE Lin.2013.The Metallogensis, Deposit Model and Prospecting Direction of the Ga’erqiong-Galale Copper-gold Ore Field, Tibet[J].Acta Geoscientica Sinica,34(4):385-394.
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