摘要
罗村斑岩体呈岩株产出,由内带、中带和外带三部分组成,不同地段岩性有所差异。通过对大量钻探资料的分析研究,认为矿床成因是与罗村燕山期斑岩体密切相关的高-中低温热液型钼、铜、铅、铁多金属矿床。
Luocun porphyry body is exposed in stock,which is composed of inner,middle and outer belts with different lithology.Based on the study of drilling data,it is believed that it is a molybdenum,copper,lead,iron polymetal deposit of high-moderate-low temperature hydrothermal type.The deposit genesis is closely related to Yanshannian prophyry body in Luocun.
出处
《矿产与地质》
2010年第4期328-331,299,共5页
Mineral Resources and Geology
关键词
钼矿
岩体特征
矿床成因
罗村
河南
molybdenum deposit
porphyry body characteristics
deposit genesis
Luocun
Henan
