摘要
银洞坡金矿位于桐柏地区北秦岭构造带,围山城金银多金属成矿带中部。矿床成因类型为变质岩来源热液型金矿床。矿床受背斜轴部构造和地层的双重控制,推断在已知矿体的深部和外围有不完全受层位控制的盲矿体存在。
Yindongpo gold deposit locates in the middle of Weishancheng Au-Ag polymetallic ore belt, North Qinling tectonic belt in Tongbai area. It is metamorphic rock from hydrothermal gold deposits. The ore deposit is controlled by anticlinal axis and stratum, so we infer that there exist blind ore bodies without completely controlled by the strata in the depth and periphery of known ore bodies.
出处
《资源导刊》
2016年第S1期16-19,共4页
Resources Guide
关键词
金矿
成矿规律及找矿方向
桐柏县银洞坡
gold deposit
metallogenic regularities and prospecting direction
Yindongpo
Tongbai County
