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贺兰山北段是中国新兴的金找矿潜力区。在分析矿体地质的基础上,结合野外地质调查,从找矿角度详细划分了区内金的成矿类型,并系统分析了断裂构造体系对成矿的具体控制作用。综合成矿构造应力场、矿体(带)空间构型及成矿流体-物质场结构分析,指出了区内下一步找矿方向,强调勘查工作应以低缓石英脉型金矿床为重点对象,兼顾F1中构造破碎带蚀变岩型金矿床。

Northern part of Helan Mountain is the emerging region for gold exploration with great potentials in China .The study carefully made out mineralization types existent in the district and systematically analyzed the specific ore-controlling effects fracture structure had on mineralization , with the help of geological analysis of orebodies and field investigation .Bringing the structural analysis of tectonic stress field ,spatial structure of orebodies and ore-forming material field-fluid field into consideration , the paper points out the low and moderately inclined quartz vein as the main exploration target and altered rock type gold deposits in structural fracture zone of F 1 also as important areas .

参考文献

[1] 李红宇,宋新华,郭合伟,孙文坤,谷守江,张连昌,黄世武,陈志广.宁夏贺兰山北段牛头沟金矿地质地球化学特征和矿床成因探讨[J].地质与勘探,2010(06):1036-1044.
[2] 宁夏回族自治区地质矿产厅.宁夏回族自治区区域地质志[M].北京:地质出版社,1990
[3] 宋新华,李红宇,郭合伟,张连昌,孙文坤,谷守江,陈志广,张晓静.贺兰山北段牛头沟金矿区围岩的原岩恢复、时代及其地质意义[J].岩石学报,2010(05):1625-1632.
[4] 耿元生,周喜文,王新社,任留东.内蒙古贺兰山地区古元古代晚期的花岗岩浆事件及其地质意义:同位素年代学的证据[J].岩石学报,2009(08):1830-1842.
[5] 黄喜峰,钱壮志,吴文奎,孙保平,逯东霞,王成,陆彦俊.贺兰山小松山基性-超基性杂岩体岩石地球化学特征[J].地球科学与环境学报,2008(04):351-356.
[6] 潘桂棠,肖庆辉,陆松年,邓晋福,冯益民,张克信,张智勇,王方国,邢光福,郝国杰,冯艳芳.中国大地构造单元划分[J].中国地质,2009(01):1-28.
[7] 邵军 .中国石英脉型金矿床地质特征[J].贵金属地质,1998,7(03):172-179.
[8] 杨春福 .辽宁五龙金矿容矿断裂构造与金矿体空间赋存特征[J].黄金,1998,18(03):3-8.
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