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广东韶关市梅子冲矿床位于南岭成矿带中段北缘一六矿区。自20世纪50年代以来,便有许多地质工作者对该矿区进行过勘查工作(裴太昌,1990;吴桂捷等,1994)。但对梅子冲矿床的研究鲜有报道。本文拟通过该矿床的矿物组合和流体包裹体特征研究,来探讨矿床成因,为进一步找矿勘探提供地质依据。矿区位于曲仁盆地南西缘,粤北山字形构造马蹄形地盾东段南侧,大东-贵东东西复杂构造岩浆带北侧,韶关-仁化新华夏构造带西侧。矿区地层主要由上泥盆统天子岭组、帽子峰组和下石炭统孟公坳组、石磴子
Shaoguan City, Guangdong plum Chong ore deposit is located in the northern margin of the middle reaches of Nanling metallogenic six ore. Since the 1950s, many geologists have conducted exploration work in this mining area (Pei Taichang, 1990; Wu Guijie et al., 1994). However, there are few reports on the research of plum Chong ore deposit. This article intends to explore the genesis of the deposit through the study of mineral assemblages and fluid inclusions in this deposit and provide the geological basis for further prospecting exploration. The mining area is located in the southwestern margin of the Qurren Basin, south of the eastern section of the northern Guangdong-Beijing mountain shaped horseshoe-shaped shield, north of the Dadong-Guidong complex structural magmatic belt, and west of Shaoguan-Renhua New Huaxia structural belt. The strata of the mining area are mainly composed of the Upper Devonian Tianziling Formation, the Hatzengfeng Formation and the Lower Carboniferous Menggongao Formation,