切特木斯铜(银)矿地质特征研究——兼论伊斯基里克地区“鸡窝”状矿体成因  

Study on geological characteristics of the Qietemusi Cu(Ag) deposit——Discussion the genesis of henroost-like orebodies in Yisijilike area concurrently

作　　者：肖力[1] 李汉光[2] 董刚[1] 金宝义[1] 唐明国[1] 韩先菊[1] 

机构地区：[1]武警黄金地质研究所,北廊坊065000 [2]武警黄金第三总队,成都610000

出　　处：《矿产与地质》2009年第4期329-334,共6页Mineral Resources and Geology

基　　金：国土资源大调查项目基金资助(项目编号:200310200014)

摘　　要：在分析切特木斯铜(银)矿的地质特征、围岩蚀变特征、矿床成因基础上,通过与典型角砾岩型矿床和典型斑岩型矿床矿化特征、蚀变特征进行对比,认为该矿床成因类型为斑岩型。根据此类型矿床找矿标志和控制因素,结合区域地质条件研究对比,初步分析了找矿方向,圈定找矿远景区。Based on the analysis of geological characteristics, wall rocks alteration and metallogeny of the Qietemusi Cu （Ag） deposit, the study believed that the studying deposit is a porphyry-host deposit after comparing the mineralization and alteration of the Qietemusi deposit with that of typical breccia-host deposit and porphyry-host deposit. According to the prospecting criteria and ore-controlling factors of this kind of deposit, the study has preliminarily analyzed prospecting direction and delimitated the perspective area for prospecting in the studying area combined with the comparison of regional geological conditions.

关 键 词：铜(银)矿 角砾岩筒 斑岩型矿床 伊斯基里克成矿带 

分 类 号：P618.43[天文地球—矿床学] P618.52[天文地球—地质学]