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丰山铜矿原是一个中型夕卡岩铜矿。近年来,通过矿山生产和有关单位研究,发现该矿床兼有斑岩铜矿和夕卡岩铜矿的地质—地球化学特征。这为丰山矿区及鄂东地区的找矿提供了新线索。矿区地质概况矿区位于淮阳山字形构造弧顶部位,主要构造为一系列北西西向紧密褶皱,地层为中下三迭统灰岩。丰山岩体出露面积约。.73平方公里,在地表呈纺睡状产出,延长方向与构造线一致。岩休主体部分为花岗闪长斑岩,边部有石英二
Fengshan Copper Mine was originally a medium-sized skarn copper mine. In recent years, through the study of mine production and related units, it has been found that the deposit has both the geologic-geochemical characteristics of porphyry copper deposits and skarn deposits. This provides a new clue for prospecting in Fengshan and Erdong areas. Mine Geological Survey Mining area is located in the Huaiyang Shan-shaped tectonic arc roof, mainly composed of a series of North West-West tight folds, the middle and lower Triassic limestone. Fengshan rock exposed area of about. .73 square kilometers, was spun out on the surface of the output, consistent with the extension of the tectonic line. Rock off the main part of granodiorite porphyry, the edge of quartz two