摘要
本文通过研究内蒙乌奴格吐山斑岩铜钼矿床及部分外围岩体矿化点包裹体研究,推测其成矿流体的演变及其与蚀变和矿化的关系,并初步探讨了外围部分矿点的含矿性.
In the light of fluid inclusion studies of the Cu-Mo-deposit in Urugetu Hill, Internal Mongolia and intrusives and mineralization occurrences in its peripheral areas, the evolution of mineralizing solution and its relation with the alteration and mineralization have been inferred. A preliminary discussion on the ore potentiality of some ore occurrences in outer areas is also given.
出处
《地质与勘探》
CAS
CSCD
北大核心
1989年第6期14-21,8,共9页
Geology and Exploration
