摘要
通过对铜官山、金口岭岩体岩石地球化学特征的分析,认为二者具有大致相似的地球化学背景,对金口岭铜金矿存在共同控矿作用;金口岭矿区几条代表性勘探线剖面钻孔资料反映,在I、Ⅱ号铜、金矿体倾向沿深部位及罗家村矿段C_(2+3)层位控制的铜铁矿体深部有进一步的找矿空间,值得关注。
Analysis of petrogeochemical features of the Tongguanshan and Jinkouling intrusions suggested that the two are roughly similar in geochemical background, which also controls the Tongjinling copper-gold ore deposit. Borehole data from several representative exploration profiles in the Jinkouling ore field indicated that ore exploration is still prospective along the deep extension of copper and gold ore bodies I and II, and in the depth of the copper-iron ore bodies controlled by C2＋3 horizon of the Luojiacun ore block.
出处
《安徽地质》
2015年第4期261-264,267,共5页
Geology of Anhui
关键词
矽卡岩型
控矿岩浆岩
层控
找矿空间
金口岭
Skarn types
ore-control magmatic rock
ore exploration space
Jinkouling
