文档介绍：找矿技术
Prospecting technology
新寨金矿区地质构造特征及找矿方向初探
吴 鹏
561000
摘 要 ：新寨金矿区位于贵州省内，地处云贵高原的东部，属低中山中切割侵蚀地貌。断裂为该矿区的主要构造，褶皱
次之。区内先后发育有近南北向、北东向及近东西向断层，并伴随断层两盘地层发育的牵引褶皱、节理、裂隙等次级构
造，这些袭次级构造部位往往是金的重要富集地段。区内断裂为主要控矿构造，构造加蚀变与金矿（化）体密切相关。本
文在以往地质勘查资料的基础上，对区内地质构造特征、矿化蚀变与矿体关系、矿床成因控制条件等进行了综合分析研
究，对区内找矿方向作出初步探讨。
关键词 ：金矿 ；地质构造；特征；矿化蚀变；找矿方向
中图分类号 ： 文献标识码 ：A 文章编号 ：1002-5065（）11-0054-2
Geological structure characteristics and prospecting direction of Xinzhai gold deposit
WU Peng
corps ofoerround Nastry Geol Explotion Buau, Anuhina)
Abstract: nai gold sit is locain Guiou Pvince, in the east of nnan iouau,nngs to
w annsion landfoult is the main structuf the ming aollowed by fold. There a
N-S, NE and EW trending faults in the area, and secondary structures such as traction folds, joints and fissures devel
o sides of the fault. These secondary structures are often important gold enrichment araults ar
ore controllincturea, and structul altera is closely rela gold minerationsed on thu
geolol eratiois pakes a comprehsive analys