红泥坡铜矿床地质特征及找矿意义  

Geological Features and Their Prospecting Significance of the Hongnipo Cu Deposit

作　　者：胡夕鹏[1] 张济礼 李世燕 杨开均 胡红波 

机构地区：[1]四川省地矿局四0三地质队,四川峨眉山市614200

出　　处：《四川地质学报》2016年第2期264-268,共5页Acta Geologica Sichuan

摘　　要：红泥坡铜矿床位于扬子准地台攀西成矿带康滇地轴中段的有色、黑色金属成矿带,矿体赋存于元古界河口群河口组及天生坝组,呈似层状、透镜状产出。本文通过对该矿床区域成矿背景、矿区地质特征、矿体地质特征、物化探特征及成矿地质条件等方面的研究,阐述了该成矿区带找矿过程、找矿意义,对寻找同类型矿床具有重要的指导意义。The Hongnipo Cu deposit is located in middle sector of the Kangdian Axis of the Yangtze Paraplatform. The deposit is confined to the Hekou and Tianshengba Formations of the Proterozoic Hekou Group. The orbodies occur as stratoid and lenticular forms. This paper deals with its regional geological setting, geological features, geophysical and geochemical expression and prospecting history.

关 键 词：铜矿 地质特征 找矿意义 红泥坡 

分 类 号：P618.51[天文地球—矿床学]