摘要
李子坪铅锌矿区分为李子坪矿段,吴底厂矿段,天生厂矿段;李子坪矿段位于矿区南部。矿体主要赋存于侏罗系中统花开左组上段破碎状泥质灰岩地层中。在研究区域地质成矿背景和矿床特征研究基础上,对矿床成因进行了分析,认为该矿床属构造控制的中低温热液矿床,并提出了5种找矿标志。
The Liziping Pb-Zn ore block is a part of the Liziping Pb-Zn deposit. The orebodies are hosted in argillaceous limestone of the Upper Member of the Middle Jurassic Huakaizuo Formation. On the basis of geological setting and geological features this paper believes that the deposit is a middle-low temperature hydrothermal one controlled by structure with 5 prospecting criteria.
出处
《四川地质学报》
2011年第3期323-325,328,共4页
Acta Geologica Sichuan
关键词
铅锌矿
矿床成因
找矿标志
李子坪
Pb-Zn deposit
ore genesis
prospecting criteria
Liziping
