摘要
通过1∶5万金牛镇、高桥镇幅区域地质调查对金牛火山岩盆地开展岩石、地层、构造、岩相、地球化学等特征的研究,认为在晚侏罗世—早白垩世期间,金牛火山岩盆地火山喷发及侵入活动强烈,断裂构造发育,具有良好的成矿地质条件,为湖北省重要的陆相火山岩铜多金属成矿远景区。
Based on 1：50000 regional geological survey,the authors study Jinniu volcanic rock basin from the aspects of rock,stratum,tectonic, lithofacies and geochemical characteristics, think there is strong volcanic eruption and intrusion activities in inniu volcanic rock basin during Late Jurassic -Early Cretaceous. Fault structure develops with good metallogenic geological conditions.
出处
《资源环境与工程》
2012年第4期313-321,共9页
Resources Environment & Engineering
关键词
金牛火山岩盆地
铜多金属
控矿因素
成矿地质背景
找矿前景
copper-polymetallic
ore-controlling factors
metallogenic background
prospecting potential
Jinniu volcanicrock basin
