小东沟钼矿床地质特征及矿床形成机制和矿床成因探讨

Discussion on Geologic Character and Metallogenic Mechanism and Formation of Xiaodonggou Molybdenum Deposit

内蒙古克什克腾旗小东沟钼矿床为次火山———热液似斑岩型矿床,钼矿体赋存于小东沟斑状花岗岩内及其内接触带上。在区域成矿地质背景下,小东沟钼矿床的形成有一定的特点,通过研究和探讨矿床的形成机制和形成原因,能够认识钼矿的成矿规律,指导找矿。

Xiaodonggou molybdenum ore is located in Ksikteng,the Nei monggol Autonomous Region,which is a similar porphyry molybdenum deposit of hypergence molten rockhydatogensis.Molybdenum-orebody is in the Xiaodonggou porphyritic granite rock and inside contactbelt. In the regional geological environment, Xiadonggo Molybdenum doposit's forming has a special feature.By investigating and discussing the metallogenic mechanism and cause of deposit formation,we can understand forming regularity of the molybdenum deposit...