摘要
本文在研究矿区的区域地质背景、矿床地质特征的基础上,依据控矿因素、矿床成因,成矿规律等,探讨了矿区成矿模式,认为矿区的主矿体位于远离岩体的外接触带,矿区的找矿工作应以侧、深部为主,深部可能存在规模较大的斑岩型和矽卡岩型盲矿体。
Based on the research area of the regional geological background, geological characteristics, ore controlling factors, according to genesis, metallogenic regularity, discusses metallogenic model, that the outer contact is located away from the main orebody mining rock belt, prospecting should be based on the side, deep, deep there may be a large scale porphyry and skarn type of blind ore body.
作者
余槐
YU Huai(Si Chuan Sheng Nucear Geology 282 Brigade,Deyang 618000,China)
出处
《世界有色金属》
2018年第3期117-118,共2页
World Nonferrous Metals
关键词
冈底斯
控矿因素
成矿模式
斑岩型和矽卡岩
Gandis
ore controlling factors
metallogenic model
porphyry and skarn