朱溪钨(铜)多金属矿床是近几年来在赣东北发现的一个超大型矿床，该矿床是由矽卡岩型、石英脉型、云英脉型、蚀变花岗岩型等4种成因类型矿体组成的“多位一体”钨（铜）多金属矿床，主要成矿元素钨、铜在空间上有明显的分带性，从北东→南西，从浅部→深部，铜含量减少，而钨含量增加。由于朱溪矿床矿体类型多、成矿多阶段，不同矿体类型的流体特征及演化规律尚不清楚，石英与白钨矿分别是朱溪矿床4种矿体类型最主要的脉石矿物与矿石矿物，是研究矿物流体包裹体的理想矿物。本项目拟在流体包裹体显微镜观察、SEM-CL图像分析基础上，结合石英、白钨矿的原位微区微量元素、氧同位素分析，以及流体包裹体的测温及单个包裹体的成分测定，研究不同类型矿体不同世代的成矿流体特征及演化规律，查明不同类型矿体的成因联系，探讨成矿元素钨铜的沉淀机制，无疑该研究对完善该矿床的成矿模式具有重要的理论意义，对该矿床深部找矿也具有一定的指导意义。

Zhuxi tungsten (-copper) polymetallic deposit is proved to be a super-larger deposit in recent years in the northeast of Jiangxi province. It consists of skarn type, quartz-vein type, greisen-vein type and altered-granite type of orebodies. The tungsten and copper are the main ore-forming elements, which are distributed with obvious zonation in space. The content of copper decreases while that of tungsten increases from NE to SW and from shallow to deep positions. Due to the multiple types of ore bodies and mineralization stages in the Zhuxi deposit, the characteristics and evolution of ore-forming fluids of different ore body types are still unclear. Quartz and scheelite are the main gangue minerals and ore minerals of the four types of ore bodies in the Zhuxi deposit, and they are ideal minerals for the study of mineral fluid inclusions. In this project, the microscopic observation of fluid inclusions, the image analysis by SEM-CL, trace elements and oxygen isotope analysis of quartz and scheelite by LA-ICP-MS and SIMS, temperature measurements of fluid inclusions and composition determinations of individual inclusion will be carried out. The aims are to better understand characteristics and evolution of ore-forming fluids of different types of ore bodies in different generations, genetic relation of different types of ore bodies and the precipitation mechanism of the tungsten and copper. This study is of great theoretical significance for improving the metallogenic model and is of great guiding significance for the deep orebodies prospecting of the deposit.