摘要
安陆同兴店铜矿位于襄广断裂北侧,处于大狼山穹窿构造中的外带,受构造和层位控制。铜矿体产于下寒武统底部黑色岩系碳酸盐岩与碎屑岩间滑脱拆离带中,小而多,呈北西向展布,平均含铜1.67%,富含银。矿石为氧化矿石,孔雀石化强烈。安陆同兴店铜矿是下寒武统底部含多金属黑色岩系中的典型矿床之一,具有重要的找矿指示意义。
Tongxingdian copper mine in Anlu City, located the north of Xiangguang fracture and outlying areas of Dalanshan domal structures,is controlled by structure and stratigraphical position. Copper orebodies, developed in slide detachment belt between carbonate rocks of Lower Cambrian black rock series and clastic rocks in northwestern extension, are small scale and numerous,with average 1.67% copper and silver-rich. The ore is oxidized ore which appear to be extraordinary high malachite mineralization. Tongxingdian copper mine is typical mineral deposit in Lower Cambrian black rock series ,with great significance in prospecting.
出处
《资源环境与工程》
2009年第4期396-400,共5页
Resources Environment & Engineering
关键词
同兴店
铜矿
基本特征
Tongxingdian
copper mine
basic characteristics
