摘要
湖北金牛火山岩盆地中生代岩浆活动经历了晚侏罗世—早白垩世初期的岩浆侵入—火山初始爆发—间歇、白垩纪的鼎盛—减弱—衰亡多个发展阶段。通过地质、物探、化探、遥感等多种找矿信息综合分析研究,在中生代火山岩区划分出1处A级铜多金属成矿远景区、1处B级铜金成矿远景区,圈定1处隐伏铜多金属矿找矿靶区,建立了吴伯浩铜多金属找矿预测模型。
The Mesozoic volcanic magmatism experienced multiple stages of development,including magmatic intrusion of the Late Jurassic to initial stage of the Early Cretaceous,volcanic initial eruption-intermittent,and the peak-weakened-de-clined of the Cretaceous in the Jinniu basin. Through geological,geophysical,geochemical and remote sensing information comprehensive analysis of a variety of prospecting,the authors identify one Class A copper polymetallic prospective area,one Class B copper-gold prospective area and one concealed copper polymetallic target area and build a prediction model.
出处
《资源环境与工程》
2014年第5期617-621,共5页
Resources Environment & Engineering
基金
中国地质调查局国土资源大调查项目(1212010610710)
