摘要
贵州水城县银硐沟铅锌矿床位于扬子陆块南部六盘水叠加褶皱带。已查明三条矿体呈脉状、透镜状均分布于北西-南东向F6断层、F7断层破碎带中,构造控明显;矿体赋矿地层为石炭系、二叠系的灰岩、白云岩;矿床成因类型为受地层岩性-构造控制的低温热液型矿床。沿F6断层和F7断层走向延长方向及倾向延深(深部)方向可作为下一步找矿的两个重点靶区。
Yindonggou Pb-Zn deposit in Shuicheng, Guizliou is in Liupanshui superimposed fold zone of SYangzi land massif. 3 veined, lenticular ore bodies have been discovered in the fractured zone of fault F6, F7with structure control clear. The ore-bearing strata are C,P limestone, dolomitite. The low T hydrotliermal deposit in genesis controlled by litliologic character and structure. The strike and dip （ deepextension） direction of fault F6, F7 can be considered to be the focus in the future prospeting working.
作者
张羽洋
王新富
ZHANGYu-yang;WANG Xin-fu(Guizhou Geoexploration Bureau o f Nonferrous and Nuclear Industry,Guiyang 550005;College Land Resources,Kunming University of Science and Technology,Kunming 650093)
出处
《云南地质》
2018年第3期325-331,共7页
Yunnan Geology
基金
云南羊拉铜矿床石英斑岩脉流体包裹体研究(编号:2017M20162101054)
关键词
构造控矿
低温热液型矿床
贵州水城银硐沟
Ore Control of Structure
Low T Hydrothermal Deposit
Yindonggou
Shuicheng
Guizhou
