摘要
茶里岩铅锌多金属矿床位于著名的香花岭矿田南部,是南岭多金属成矿带的重要组成部分。笔者通过野外地质工作、综合整理和分析研究。总结了区内的成矿地质条件、控矿因素等特征,确定矿床成因类型为中-高温热液裂隙充填型矿床,矿床规模为中型。从研究香花岭矿田内各大中型矿床的矿化类型,结合工作区地质条件,提出了本区的找矿方向及前景。
The Chaliyan Pb-Zn-polymetallic deposit lies in the famous Xianghualing ore field which is an important part of the Nanling polymetallic metallogenic belt. This paper deals with ore-forming geological conditions, ore control factors and deposit type of the deposit. The Pb-Zn-polymetallic deposit is a medium-sized meso-and hypothermal and fissure filling deposit. The range of reconnaissance and prospecting potential are put forward.
作者
肖颖斌
黎原
易元顺
黎传标
XIAO Ying-bin;LI Yuan;YI Yuan-shun;LI Chuan-biao(China University of Geosciences(Beijing),Beijing 100083;South Hunan Institute of Geological Survey,Chenzhou,Hunan 423000)
出处
《四川地质学报》
2020年第1期40-44,共5页
Acta Geologica Sichuan
基金
湖南省探矿权采矿权价款项目“湖南省临武县茶里岩矿区铅锌多金属矿普查”资助.
