斑岩型钼矿床研究进展  

Advances in study of porphyry molybdenum deposits

作　　者：简伟[1] 柳维[1] 石黎红 

机构地区：[1]中国地质大学地球科学与资源学院,北京100083 [2]河南省灵宝市地质矿产局,河南灵宝472500

出　　处：《矿床地质》2010年第2期308-316,共9页Mineral Deposits

基　　金：全国危机矿山接替资源找矿项目(20089949;200841019);国土资源大调查项目(1212010634001);国家自然科学基金项目(40434011)的联合资助

摘　　要：文章总结了北美西部及中国斑岩型钼矿床的研究成果,介绍了斑岩型钼矿床的分类、共生岩浆岩、矿化方式及蚀变特点,重点探讨了斑岩型钼矿床的成矿流体特点,钼在岩浆-热液系统中的富集沉淀机制以及斑岩型钼矿床的成矿物质来源。Porphyry molybdenum deposits, the most important molybdenum resources in the world, are spatially, temporally and genetically associated with porphyritic intrusions. Based on a summarization of researches on porphyry molybdenum deposits in western Cordillera of North America and China, this paper deals with such aspects of porphyry molybdenum deposits as their classification, co-genetic igneous rocks, mineralization and alteration characteristics, with the emphasis placed on transportation and deposition of molybdenum, characteristics of ore-forming fluids, and sources of magmas and metals of these deposits.

关 键 词：地质学 斑岩型钼矿床 Climax型钼矿床 特征 流体 富集 沉淀 物质来源 综述 

分 类 号：P618.65[天文地球—矿床学]