摘要
枪马金矿位于河南省灵宝市,矿床产出受太华群变质岩、岩浆岩和构造等多种因素的控制。金矿体以石英脉型为主,次为蚀变岩型,矿体在倾向上和走向上均具有尖灭再现的特点,并具有向SE侧伏的规律。枪马金矿区的深部具有较好的成矿前景和找矿潜力。
Qiangma gold deposit is located in Xiaoqinlign region,Lingbao, Henan. Taihua group metamorphic suites, magmatic rock and tectonics control the occurrences of the gold deposit. The quartz vein is main type of the gold ore and then alterated catactastic rock type. The gold ore body is characterized by repeated pinching-out and re-appearance both along dip and strike and by pitch to southeast. The oreforming process is displayed to depth and it is potential for further exploration in Qiangma mine area.
出处
《地质找矿论丛》
CAS
CSCD
2010年第3期223-227,245,共6页
Contributions to Geology and Mineral Resources Research
关键词
枪马金矿
矿床地质特征
深部找矿潜力
河南省
Qiangma gold deposit
quartz vein type
geological characteristic of deposit
exploration potentiality for the deep levels
Henan province
