本项目拟以新疆西天山地区色勒特果勒还原性斑岩-矽卡岩型Cu-Mo矿床及其矿化斑岩为主要研究对象，在野外地质、热液蚀变分带、矿化类型划分、岩石和矿物组构特征和前期预研究的基础上，开展系统的元素、同位素、矿床和流体地球化学研究，以便确定该矿床热液蚀变和矿化斑岩地球化学特征，厘清热液蚀变类型、热液矿物组合和矿化阶段的特征及其他们之间的相互关系，建立该矿床的热液矿物生成顺序表，探讨该矿床形成的构造背景，核实该矿区斑岩体是否都具有还原性钙碱性I型花岗质岩石的特征并探讨其成因，特别要重点探讨富CH4的还原性成矿流体的来源与演化、成矿流体中的CH4来源及其对铜、钼成矿作用的影响等，建立该矿床的成矿模式，完善还原性斑岩矿床的成矿理论。

The Seleteguole reduced porphyry-skarn Cu-Mo deposit in Jinghe County, Xinjiang, China and the mineralized porphyries are selected as main research objects of this proposal. On the basis of field geology, hydrothermal alteration zoning, classification of mineralization types, textural and structural characteristics of rocks and minerals, and our previous geochamical pre-research of the deposit, a series of systematic elemental geochemistry, isotope geochemistry, ore deposit geochemistry, and fluid inclusion study will be undertaken in this proposed project, to confirm the geochemical characteristics of the hydrothermal alteration and mineralized porphyries of the deposit, to clarify types of hydrothermal alteration, characteristics and relationships of hydrothermal mineral assemblages and mineralization stages, to establish sequence of hydrothermal mineral formation of the deposit, to discuss tectonic background of the metallogeny of the deposit, to verify whether porphyries of the deposit are characterized with reduced calc-alkaline I type granitoids and then to discuss genesis of those porphyries, to especially probe the origin and evolution of the CH4-rich reduced ore-forming fluid, the origin of the CH4 in the ore-forming fluid and its influence on the Cu and Mo mineralization of the deposit, then to establish the metallogenic model of the deposit, and finally to consummate metallogenic theory of the reduced porphyry deposit.