从凤太矿田找矿历史谈找矿方向  

From the Fengtai Ore Prospecting Direction of History

作　　者：张耀斌 姚善杰 王双彦 任存莲 张淑玲 张选固 

机构地区：[1]西北有色地质勘查局七一七总队,陕西宝鸡721015

出　　处：《甘肃冶金》2016年第1期103-105,共3页Gansu Metallurgy

摘　　要：凤太矿田找矿历史有记录以来从上世纪五十年代至今已有近六十年的历史,最早是岩浆热液成矿论,发展到层控、海底喷流学说。控矿因素也是由最早的岩相地层控矿,发展到现在的背斜控矿理论。事实上找矿主要靠的是控矿因素和空间展布特征,而不是矿床成因。从凤太矿田分布有大量的隐伏背斜来看,找矿仍有很大的空间,未来找矿方向应从寻找隐伏背斜入手,把复杂的找矿变成简单的寻找背斜,在背斜构造环境内圈定成矿有利部位是找矿的捷径,便于操作,也会收到事半功倍的效果。Feng Tai orefield find mine historical records from the fifties of the last century has been nearly 60 years of history,the earliest is magmatic hydrothermal metallogenic theory,development to stratabound submarine exhalative theory. Ore controlling factors are also the earliest exploration of lithofacies,and the development of the current theory of the control of ore deposits. In fact,it is mainly controlled by ore controlling factors and spatial distribution characteristics,but not the genesis of ore deposits. From the perspective of the Fengtai ore field distribution of a large number of concealed anticline,prospecting there are still a lot of space,future looking for ore from the direction of searching for concealed Anticline of,the complex ore into simple find anticline,in anticline tectonic environment of inner ring fixed favourable metallogenic position is a shortcut for ore prospecting. Easy to operate,it will receive a multiplier effect.

关 键 词：凤太矿田 找矿历史 矿床成因 控矿因素 

分 类 号：P622[天文地球—地质矿产勘探]