铜绿山矿田成矿远景预测及三维地质模型

刘豹, 杨宇山, 刘天佑

Metallogenic prospect prediction and 3D geological modeling for the Tonglyushan ore field

LIU Bao, YANG Yu-Shan, LIU Tian-You

图1 铜绿山矿田区域构造(a)及地质(b) F1—鄂城-咸宁超壳断裂;F2—襄樊-广济超壳断裂;F3—姜桥-下陆断裂;F4—江南带断裂;F5—毛铺-两剑桥断裂;F6—山坡-枫林超壳断裂;X1—大冶湖向斜;Y1—鄂城岩体;Y2—铁山岩体;Y3—金山店岩体;Y4—灵乡岩体;Y5—殷祖岩体;Y6—阳新岩体;L01~L55—反演的55条剖面位置

Fig.1 Regional teotonic map (a) and geological map (b) of Tonglyushan ore field F1—Echeng-Xianning supershell fault;F2—Xiangfan-Guangji supershell fault;F3—Jiangqiao-Xialu fault; F4—Jiangnan Belt fault;F5—Maopu-Liangjianqiao fault;F6—Shanpo-Fenglin supershell fault;X1—Daye Lake syncline;Y1—Echeng rock mass;Y2—Tieshan rock mass;Y3—Jinshandian rock mass;Y4—Lingxiang rock mass;Y5—Yinzu rock mass;Y6—Yangxin rock mass;L01~L55—represents 55 sections for inversion