乌奴格吐山斑岩铜钼矿床流体包裹体与成矿作用研究  

A Study on Fluid Inclusion and Metallogenesis of a Porphyry Cu-Mo Deposit, Urugetu Hill, Inner Mongolia, China

作　　者：叶欣[1] 王莉娟[1] 

机构地区：[1]中国有色金属工业总公司北京矿产地质研究所

出　　处：《地质与勘探》1989年第6期14-21,8,共9页Geology and Exploration

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.

关 键 词：斑岩 铜钼矿 液包体 矿化作用 

分 类 号：P618.650.5[天文地球—矿床学]