| 斑岩型钼矿床研究进展 |
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| 引用本文：石黎红.2010.Advances in study of porphyry molybdenum deposits [J].Mineral Deposits,29(2):308~316 |
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| 基金项目:?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）和国家自然科学基金项目（40434011） |
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| 中文摘要: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。 |
| 中文关键词: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 |
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| Advances in study of porphyry molybdenum deposits |
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| Abstract:Porphyry molybdenum deposits, the most important molybdenum resources in the wor ld, are spatially, temporally and genetically associated with porphyritic intrus ions. Based on a summarization of researches on porphyry molybdenum deposits in western Cordillera of North America and China, this paper deals with such aspect s 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 flui ds, and sources of magmas and metals of these deposits. |
| keywords:geology, porphyry molybdenum deposits, Climax-type molybdenum deposits, characteristics, fluids, concentration, deposition, sources, review |
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