与花岗岩有关的W钨矿床是最重要的矿床之一，其金属组合多样，前人对W-Sn-Nb-Ta成矿系统的成因机制有很较深入的研究和认识。然而，对W-Cu成矿系统研究相对较薄弱，尤其是动力学机制、岩浆成矿作用机制和成矿物质来源等科学问题亟需厘定。以W-Cu特殊组合为特征的赣北朱溪和大湖塘矿床，成矿规模巨大，地质构造背景完全不同于著名的W矿基地—南岭成矿带，其构造分区、成矿岩体的岩石归类属性及成矿作用机制、成矿物质来源尚存在争议，且两个矿床均发现直接代表岩浆-热液过渡阶段的伟晶岩壳。因此，本文拟选取朱溪和大湖塘两个矿床，针对上述科学问题，联合运用大数据分析、矿物学-岩石学-地球化学分析测试、同位素示踪和流体包裹体显微测温等手段，反演赣北地区W、Cu超级富集过程与就位机制。研究将完善W矿床W、Cu超常富集过程的理解，为建立华南W矿勘查提供重要支持，具有重大科学意义。

As one of the most important metal resources, granite-related tungsten deposits show complicated metal series from W, W-Sn, W-Mo, W-Sn-Nb-Ta and W-REE, and have been comprehensively studied by geologists for a long time. However, the W-Cu deposits are rarely mentioned, especially on the regional tectonodynamics, mechanism of magmatic mineralization and origin of the ore-forming material including W and Cu. The two superlarge newly-discovered deposits Zhuxi and Dahutang W-Cu are located in the north Jiangxi province, which belongs to the superimposed part of foreland nappe thrust zone of the southeast coast of Eurasian continental Plate, and the Precambrian Suture between the Yangtze and Cathaysia Plates. The granites in the two deposits are complicated multiphase intrusions and their roles on the metallogenesis of tungsten an copper are unclear. And the pegmatite veins or shells, which represent the direct product of the transporation from magma to hydrothermal fluid, have been found out in the two deposits. Therefore, Zhuxi and Dahutang are selected to study in this paper to recipher mechanism and process of the hypernormal transportation and enrichment of W and Cu through Big data analysis, mineralogical, petrological and geochemical measurement, isotopic tracing, and fluid inclusions microthermometer and calculation. It will also show light on the tungsten prospecting in South China.