摘要
金龙山金矿区的空间展布严格受背斜和断裂的控制,其中北东向断裂为主要控矿断裂,尤其在背斜核部和断裂交汇处易形成厚大矿体。因此,在强短轴背斜和断裂构造及交汇处是成矿的有利构造条件,本文通过对成矿地质条件的分析表明,在矿床深部及外围具有较大找矿潜力。
The spatial distribution of Jin Long Shan goldmining area is strictly controlled by the anticline and fracture.The NE-trending fault is the main ore-controlling fracture,particularly in the intersection of anticline core formation and fracture formed the huge ore body easily.Therefore,it is more beneficial to mineralized.By analyzing the ore-forming geological conditions,the result shows that it has more potential for mineral prospecting in the deep and external deposits.
出处
《有色矿冶》
2009年第5期4-7,共4页
Non-Ferrous Mining and Metallurgy
关键词
成矿地质条件
矿床成因
找矿潜力
金龙山矿区金矿床
the ore-forming geology condition
mineral deposit cause of formation
further exploration
Jin Long Shan mining area gold deposit
