摘要
该矿床位于沂沭断裂带东侧,其大地构造位置属华北板块(Ⅰ)、胶辽隆起区(Ⅱ)、胶北隆起(Ⅲ)、胶北断隆(Ⅴ)、明村-但山凸起(Ⅵ)西南部。具有良好的地质成矿条件和找矿远景。本文着重点在于通过对矿区矿床(体)地质特征的分析,阐明矿体赋存特征,研究矿床成因。
With the deposit is located in the east of the Yishu Fault, the tectonic location is North China plate(I), Jiaoliao uplift(II) and(III) jlaobel uplift, Jiaobei uplift(V), Ming Village-but the mountain uplift(VI) southwest. It has good geological and metallogenic conditions and prospecting prospect. This paper focuses on the analysis of geological characteristics of ore deposits(bodies) in the mining area, and expounds the occurrence characteristics of the ore bodies and studies the causes of the deposits.
出处
《世界有色金属》
2017年第16期200-200,202,共2页
World Nonferrous Metals
关键词
矿床
地质特征
沉积变质
deposit
geological characteristics
sedimentary metamorphism