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赣北大湖塘超大型钨矿区产有石门寺、狮尾洞、大岭上、东陡崖等一系列大中型与燕山期花岗岩体密切相关的钨铜(钼)多金属矿床。前人仅张婉婉(2012)和Gong et al.(2015)分别报道过大岭上和石门寺流体包裹体的相关研究,但样品均主要为石英脉。为系统地研究大湖塘钨矿床的成矿流体特征,本文对与三大类型矿体(隐爆角砾岩型、石英大脉型、细脉浸染型)密切共生的石英及成矿母岩-白云母花岗岩开展详细的流体包裹体岩相学、显微测温、及包裹体拉曼测试工作,旨在讨论成矿流
The Dahuntang ultra-large tungsten ore district in northern Jiangxi produces a series of tungsten-copper (molybdenum) polymetallic deposits closely related to the Yanshanian granite body such as Shimenji, Ligongdong, Dalingshang and East Steep Cliffs. Previous studies by Zhang Wan-wan (2012) and Gong et al. (2015) respectively reported fluid inclusions in the Dalingshang and Shihmen temples, but the samples were mainly quartz veins. In order to systematically study the characteristics of ore-forming fluid in the Dahuntang tungsten deposit, the paper deals with the quartz and ore-forming parent rock closely intergrowth with the three major types of ore bodies (cryptoexplosive breccia type, quartz vein type and vein disseminated type) The muscovite granitoids carry out detailed fluid inclusions petrography, microscopic temperature measurement, and inclusion Raman tests to discuss the ore-forming fluid