矽卡岩型白钨矿床是最重要的钨矿床之一，岩浆热液是W迁移、沉淀的重要控制因素。然而，关于热液组分（F-、Cl-、Na/Ca金属阳离子、CO2-等）对矽卡岩型白钨矿床W-Cu沉淀的控制作用存在争议，阻碍了人们对矽卡岩型白钨矿床成因的理解。朱溪W-Cu矿床是华南新发现的与区内燕山期花岗岩有关的特大矽卡岩型白钨矿床，其成因研究处于起步阶段，与典型的矽卡岩型白钨矿床成矿地质特征类似，而且该矿床以钨铜为组合特征，明显区别于南岭地区以钨锡、钨钼组合为主的钨矿床，另外，朱溪钨铜矿床的发现与赣东北地区以铜钼金为成矿特点相悖，需要重新认识赣东北及相邻区域地质背景、区域成矿规律及其对钨矿的控矿作用。为此，本课题拟选取朱溪W-Cu矿床开展流体成矿作用研究，理清流体组分特征及其对W、Cu沉淀的控制机制，确定W、Cu来源及沉淀机制，并结合已有的成因模式和解释，解析矽卡岩型白钨矿床成因，为钨矿床勘查找矿提供理论依据。

Skarn scheelite deposit is one of the most significant types of Tungsten Deposit in the world. Its metallogenesis is seriously restricted by geochemical features of granites, composition of wall rocks, forming depth of mineralization and alteration, and redox condition and temperature variation of metallogenic system. However, effect of hydrothermal components on tungsten precipitation is unclear. The newly discovered Zhuxi deposit is a giant skarn scheelite deposit related with granites. All its ore bodies are restricted above the contact zone of Neoproterozoic metasedimentary rocks and Paleozoic carbonate rocks and many F-rich minerals such as vesuvianite, fluorite and muscovite could be observed in the skarn mineral assemblages. What's more, lots of chalcopyrite grows altogether in the Zhuxi deposit so that the copper resource adds up to over 10 Wt. All of the above characteristics made the Zhuxi deposit very suitable to carry out genesis research so as to find out the ore-forming mechanism of the skarn scheelite deposit and its significane on precipitation of tungsten and copper. Additionally, the Zhuxi tungsten deposit was located in the northeastern Jiangxi Province, where tungsten deposit had never been discovered and all geological research and mineral exploration had been completely focused on the metal including Cu, Mo, An and Pb-Zn before. It is unclear how the tectonics, regional sedimentary rocks and magmatism influence the tungsten mineralization. Therefore, a typical metallogenesis research on the fluid inclusions and its significance on tungsten and copper precipitation stable isotopes, as well with comparative analysis of different sorts of tungsten deposits in the Nanling area and typical scheelite Skarn-type depsosits in other countries, will be carried out in this paper, to make clear the mechanism of skarn scheelite deposits, the factors affected the precipitation of scheelite and chalcopyrite, and regional metallogenic regularity in South China.