基于汤中立提出的“小岩体成大矿”的事实与理论认识~([1,2]),传统的岩浆热液成矿理论对某些矿床的成因并不能给出很好的解释~([3]),小体积岩体无法析出导致大规模成矿作用的流体和金属已经得到证实~([4,5])。罗照华等~([3])从“小岩体成大矿”的角度切入,对该理论进行了系统验证及阐述,提出了透岩浆流体成矿作用理论的框架模型,论证了该理论模型在研究现代成矿作用机制等方面所具有的重要现实意义。甭哥碱性杂岩体所在区域一直以来被认为是滇 Based on the factual and theoretical understanding of the “small rock mass into a large ore” proposed by Tang Zhongli, the traditional magmatic hydrothermal mineralization theory does not give a good indication of the genesis of some ore deposits Interpretation ~ ([3]), small volumes of rock can not be precipitated lead to large-scale metallogenetic fluids and metals have been confirmed ~ ([4,5]). Luo Zhaowa, et al ~ ([3]) cut from the perspective of “small rock mass into large ore”, systematically verified and elaborated this theory, put forward a framework model of the theory of metallogenic action of trans-magmatic fluid, and demonstrated that this theory Model in the study of the mechanism of modern mineralization has important practical significance. The area where the Gejiu alkaline complex is located has long been regarded as Yunnan