摘要
庙山金矿位于秦岭造山带西秦岭中部花岗岩带,属北中秦岭陆表海盆中段。赋存于高桥—洮坪大断裂西段。通过对金矿体地质及矿带特征较为客观认识的基础上,分析总结矿体控矿因素指导深部探矿。经深部坑探,矿体氧化深度较深(最深178m),矿体向深部有变富变厚的趋势。庙山金矿属断裂破碎带控制的中低温热液蚀变岩型金矿。
Miaoshang gold deposit exists in the granite zone of the middle part of west Qinling. It is a middle-low hydro-thermal type gold deposit controlled by the fracture zone of Gaoqiao-Taoping Fault. The paper analyzed geological features of ore bodies and metallogenetic zone, and summarized the ore control factors. The study show that the ore body has the trend of richer and thicker towards deeper.
出处
《甘肃地质》
2013年第3期41-45,共5页
Gansu Geology
基金
核工业地质局基金项目:庙山金矿详查项目
关键词
地质特征
控矿因素
庙山金矿
geological characteristics
ore-control factors
Miaoshan gold deposit
