海城市范家堡子滑石矿床外围找矿预测  

Prospecting target around Fanjiapuzi talc deposit in Haicheng City

作　　者：何忠波[1] 王嵩莉[2] 王东波[1] 何伟[1] 姜福伦[1] 

机构地区：[1]辽宁省第五地质大队,辽宁营口115100 [2]吉林大学应用技术学院,吉林长春130022

出　　处：《吉林地质》2009年第3期52-55,共4页Jilin Geology

摘　　要：简单地介绍了矿床地质特征,详细地分析了矿床的构造特征,推测矿区为一北北东向—倒转向斜的一部分,在F2断层的东侧已控制矿体的下部倒转向斜的核部和另一翼为本区的找矿方向。Geologic features of the talc deposit are introduced simply, and structure features of the talc deposit are analysed in detail.by inference,the mining area is a part of an overturned syncline which is strike direction in northeast by north, prospecting target around talc deposit within mining area is the core of overturned syncline under measured ore body and the other flank of overturned syncline on the east of F2 fault to the east.

关 键 词：地质构造 倒转向斜 找矿方向 滑石矿床 

分 类 号：P619.253[天文地球—矿床学]