里伍铜矿田控矿构造特征与找矿方向  

Ore-controlling structure and prospecting direction of liwu copper mine

作　　者：杨光源[1] 余祥龙 王昌南[1] YANG Guang-yuan;YU Xiang-long;WANG Chang-nan(Sichuan Liwu Copper Co., Ltd., Ganzi 626200,China)

机构地区：[1]四川里伍铜业股份有限公司,四川甘孜626200

出　　处：《世界有色金属》2019年第1期166-167,共2页World Nonferrous Metals

摘　　要：里伍铜矿田位于江浪变质核杂岩穹隆的构造结构中,目前已经发现了很多中小型的铜矿床,包括里伍,黑牛洞等,也被作为是西缘地区铜矿的集中产地。其中中深层次的江浪变质核杂岩是该矿区的主体构造。本文我们通过对里伍铜矿的地质特点,控矿因素及构造特征进行深入分析,说明了里伍铜矿田和区域的找矿方向。The Liwu copper ore field is located in the structural structure of the Jianglang metamorphic core complex dome. At present, many small and medium-sized copper deposits have been discovered, including Liwu, Heiniudong and so on. It is also regarded as the concentrated copper deposit in the western margin. The middle-deep Jianglang metamorphic core complex is the main structure of the mining area. In this paper, the geological characteristics, ore-controlling factors and structural characteristics of the Liwu copper deposit are thoroughly analyzed, and the prospecting direction of the Liwu copper field and region is explained.

关 键 词：里伍铜矿田 控矿 构造 特征 找矿 

分 类 号：P618.41[天文地球—矿床学]