以比较矿床为指导，紧紧抓住东天山发育中生代层控钼矿床的特色，以东戈壁、白山大型钼矿床为代表，系统解剖其地质地球化学特征（特别是流体包裹体特征），确证它们为层控造山型钼矿床，提出层控造山型钼矿床的存在，拓宽找矿思路，丰富造山型矿床"家族"的成员，将国际造山型金矿床研究热潮引领到"造山型矿床"，使东天山成为国际造山型矿床研究的热点地区之一；运用多种有效的地球化学示踪技术，查明矿床成矿流体的性质和演化规律，揭示其与造山型金矿的共性和差异，找出矿化元素共生、分带规律和主控地质要素，建立成矿模型，提出攻深找盲-外围求新（新矿体、新类型）的勘查模式；精确测定成矿时代，解析矿田构造，结合大地构造研究进展，成矿与区域地质演化的时空、成因关联，完善增生体制下造山型矿床的成矿模式，构建增生体制下流体成矿理论框架，丰富和发展区域成矿理论，促进"造山与成矿"研究的进展。

The instruction of the comparative metallogeny, and tightly seize East Tianshan mesozoic stratabound characteristics of the molybdenum deposits.Research on the Donggebi,Baishan molybdenum deposits，study its geological and geochemical characteristics (especially the fluid inclusion), make sure they are one of the stratabound orogenic molybdenum deposits, this implies that East Tianshan has great potential for orogenic-type deposits. The use of a variety of effective geochemical tracer techniques to determine whether the mineral deposits to ore-forming fluid nature and evolution law, and reveal its orogenic-gold deposits.with the similarities and differences between elements, identify mineralization.symbiotic, with patterns and master geological elements, build a metallogenic model.to a deep-blind - find new exploration mode; precision dating chronology of deposits,.combined with tectonic research progress, mineralization and the regional geological.evolution of the space-time and causes hyperplasia associated under the system, and.perfect for a orogenic-type deposits of the subduction-accretion orogenic belt.model, to build a mine under the system fluid into a theoretical framework and enrich.and develop regional mineralization theory, the promotion of "orogeny and mineralization".