摘要
四川省名山地区钙芒硝矿成矿类型属晚白垩世内陆湖相—咸湖相硫酸盐沉积型,南庙沟钙芒硝矿位于川西台陷雅安穹褶束之名山向斜缓展起伏的东翼,矿体严格受白垩系上统灌口组上段地层控制。本文对南庙沟钙芒硝矿矿床成因进行了详细的分析,并总结了成矿规律和找矿标志,对本区芒硝矿的资源勘查具有重要的指导意义。
Glauberite deposit in Mingshan, Sichuan is Late Cretaceous continental lacustrine sulfate deposit The Nanmiaogou glauberite deposit lies in the east limb of the Mingshan syncline. The orebodies are controlled by the Guankou Formation. This paper makes an approach to geological features, ore genesis and ore criteria of the deposit.
出处
《四川地质学报》
2015年第3期372-376,共5页
Acta Geologica Sichuan
关键词
芒硝矿
地质特征
矿床成因
名山
glauberite
geological feature
ore genesis
Mingshan, Sichuan
