黔东南雷公山地区矿化特征及找矿前景  

THE METALLOGENESIS FEATURE AND PROSPECTING POTENTIALITY OF LEIGONGSHAN AREA IN SE GUIZHOU

作　　者：李良波[1] 吴小艳[1] 徐长昊[1] 张伟[1] 

机构地区：[1]成都理工大学地球科学学院,四川成都610059

出　　处：《云南地质》2015年第4期573-578,共6页Yunnan Geology

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.

关 键 词：矿化蚀变 韧性剪切带 构造控矿 黔东南雷公山 

分 类 号：P612[天文地球—矿床学]