摘要
南召县乔端地区铜矿成矿地质条件较好。该地区铜矿床多分布于火神庙组酸性火山岩石英角斑凝灰岩中,受断裂控制不明显,围岩具显著的热液蚀变,属火山热液沉积型块状硫化物铜矿床。本文在研究南召乔端地区多个铜矿床的第一手翔实地质勘查成果资料的基础上,总结了乔端地区铜矿床地质特征及找矿标志,并对矿床成因进行了讨论,以期对乔端地区及外围寻找铜矿床提供参考。
Ore-forming geological conditions of the Qiaodan copper deposit in Nanzhao County are good.The copper deposits are mainly distributed in the quartz corner porphyry tuff of the acid volcanic rocks of the Huoshenmiao formation,and are not obviously controlled by faults.On the basis of the first-hand detailed geological exploration data of several copper deposits in Qiaoduan area,Nanzhao County Province,this paper summarizes the geological characteristics and prospecting criteria of the copper deposits in Qiaoduan area,Nanzhao County,and discusses the genesis of the deposits,it is expected to provide a reference for the exploration of copper deposits in Qiaoduan area and its periphery,Nanzhao County,Henan Province.
作者
陈春景
王巧玲
乔海霞
杨水旺
余智慧
尚凯凯
韩姗姗
CHEN Chunjing;WANG Qiaoling;QIAO Haixia;YANG Shuiwang;YU Zhihui;SHANG Kaikai;HANG Shanshan(Henan Engineering Research Center for Non-ferrous Metal Mineral Exploration,Zhengzhou 450016,Henan,China;Henan Provincial Non-ferrous Metals Geological and Mineral Resources Bureau No.7 Geological Team,Zhengzhou 450016,Henan,China)
出处
《矿产勘查》
2022年第8期1099-1107,共9页
Mineral Exploration
关键词
铜矿床
矿床地质特征
找矿标志
矿床成因
南召乔端地区
copper deposit
geological characteristics of the deposits
prospecting marks
genesis of the deposits
Nanzhao-Qiaoduan area