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近年来在皖南的地质找矿中,取得比较大的突破的就是钨钼金矿种,邓家坞钼矿是其中之一。邢凤鸣等(1991)在皖南确定了一条晋宁早期花岗闪长岩带,它们近东西向的祁门-歙县-三阳坑断裂带分布,大小有11个岩体。邓家坞岩体就是其中之一。本次通过地球化学示踪,判断成矿岩体为陆壳成因,并对其形成的大地构造环境进行了深入的研究。1样品采集及分析方法
In recent years, geological prospecting in southern Anhui, made a relatively large breakthrough is the tungsten and molybdenum gold species, Deng Jiawu molybdenum mine is one of them. Xing Fengming et al. (1991) identified an early Jindian granodiorite belt in southern Anhui and distributed nearly Qidong-Juxian-Sanyangkeng fault zone in the east-west direction with 11 rock masses in size. Deng Jiawu rock mass is one of them. Through geochemical tracing this time, the metallogenic rock body is judged as the genesis of the continental crust, and the geotectonic environment formed by it is further studied. 1 sample collection and analysis methods