贵州册亨县板年-大沟金矿(化)区地质特征及找矿方向探讨  

Regional Geologic Characteristics and Prospecting Direction of Bnanian-Dagou Gold Deposit in Ceheng,Bannian

作　　者：方策[1] 张焕超[1] 

机构地区：[1]贵州省地矿局117地质大队,贵州贵阳550018

出　　处：《贵州地质》2011年第2期99-103,113,共6页Guizhou Geology

摘　　要：本文通过已有资料综合分析,总结描述了矿区基本地质及金矿化地质特征,提出区内F2断层应为次要的导矿构造和主要容矿构造,提出下步的找矿方向,对指导该区找矿及勘查工作具有一定意义。According to the former information,it discussed the basic geologic and gold mineralization characteristics in the mining area,the fault F2 is thought to be the secondary conducting structure and the main host structure,the further exploration direction is carried out and it will has some significance for the prospecting and exploration in this area.

关 键 词：金矿 地质特征 容矿构造 贵州 

分 类 号：P618.51[天文地球—矿床学]