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西掌金铜矿床位于云南省云县-景洪火山弧Cu多金属矿带,是与印支期中酸性次火山岩密切相关的浅成低温热液型矿床。金铜矿脉主要受近东西向构造破碎带控制,产于上三叠统小定西组第二亚段粗面玄武岩夹凝灰岩中。矿化主要集中在多期断裂构造复合与多阶段火山岩脉叠加部位。通过对西掌金铜矿区地质地球化学特征的研究,认为西掌村找矿靶区内Ⅰ号金异常具有一定的找矿潜力。

Xizhang Au-Cu Deposit is located in Yunxian-JingHong ( volcanic arc ) Cu polymetallic ore belt in Yun County ,Yunnan Province ,and is a low temperature hypabyssal hydrothermal type deposit closely related to acidic sub -volcanic rocks of indosinian period .Au-Cu veins are mainly controlled by the near EW trending tectonic fracture zone , which are found in the rough surface basalt tuff in the second sub-segment ,Xiaodingxi Group ,upper Triassic .Minerali-zation mainly concentrates in the combination of multi-phase tectonic fracture structures and the overlaps of multi-stage volcanic rock veins .

参考文献

[1] 闵毅;周晓锋;李建伟.云南省黄金资源潜力评价[M].北京:地质出版社,2010
[2] 范承钧 .区域地质调查报告书地质部分(景东幅)[R].昆明:云南省地矿局区调队,1977.
[3] 范承钧 .区域地质调查报告书矿产部分(景东幅)[R].昆明:云南省地矿局区调队,1981.
[4] 和正中 .三江中南段金及多金属矿预查报告[R].昆明:中国人民武装警察部队黄金第十支队,2012.
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