摘要
黔东南雷公山地区的金、铅锌、锑多金属矿床主要受韧性剪切带控制,从其成矿背景和成矿规律,结合区域地球物理及地球化学特征看,于矿化蚀变作用强烈的雷公山复式背斜核部及韧性滑脱构造带内,寻找深部隐伏矿体有着较好的前景。
The Au,Pb- Zn,Sb Multimetallic deposit in Leigongshan area of SE Guizhou is mainly controlled by the ductile shear zone. According to the metallogenesis setting and rule,in combination with the regional geophysical and geochemical characteristics, we think that there is the good prospecting potentiality of deep blind orebody in the intensely metallogenetic and altered core of Leigongshan anticlinorium and the ductile decollement structural zone.
出处
《云南地质》
2015年第4期573-578,共6页
Yunnan Geology
关键词
矿化蚀变
韧性剪切带
构造控矿
黔东南雷公山
Metallogenesis and Alteration
Ductile Shear Zone
Ore Control of Structure
Leigongshan
SE Guizhou
