世界有色金属Issue(7)：70-72,3.
会理县中厂矿区铜矿地质特征及成因分析
Geological characteristics and genesis analysis of copper deposits in the Zhongchang mining area of Huili County
张雄 1邱光亮 2陈彬彬1
作者信息
- 1. 四川省冶金地质勘查院,四川 成都 610051
- 2. 四川省自然资源投资集团有限责任公司,四川 成都 610051
- 折叠
摘要
Abstract
The mining area is located in the middle section of the Miyi Qiong fault bundle in the central southern section of the Kangdian axis.This area has a relatively complex tectonic movement,with folded and fractured structures developed in the region.The alteration of surrounding rocks such as silicification and dolomitization is closely related to copper deposits.The interlayer sliding zone of dolomite and marble formed by metamorphic factors in carbonate rock series is the main location for the occurrence of ore bodies and plays a significant controlling role in their production.The structure within the area is closely related to the enrichment of the ore deposit,and the ore body is mainly enriched in the lower part of the ore bearing layer.The article systematically discusses the geological characteristics of copper deposits in the Zhongchang mining area based on practice,and analyzes their genesis,in order to provide some reference for the exploration work in the area.关键词
中厂铜矿/地质特征/矿床成因/找矿标志Key words
Zhongchang Copper Mine/Geological characteristics/Origin of mineral deposits/Exploration markers分类
地质学引用本文复制引用
张雄,邱光亮,陈彬彬..会理县中厂矿区铜矿地质特征及成因分析[J].世界有色金属,2024,(7):70-72,3.
