摘要
本文通过对泗峡口地区微细浸染型金矿进行系统的研究，得出该区金矿与陕西境内的小河等金矿有极大的相似性．含矿岩系为上泥兰统南羊山组，控矿构造为层间断层、共轭剪切断层、扭性断层．金矿成因与地下热卤水有关等重要结论。
From the systematic studies, it is concluded that the micro - disseminated gold deposits in Sixiakou area extreamly similar to the same type of the gold deposits in Sbaanxi province. Their ore - bearing rock series is Nanyangshan Formation of Upper Devonian Series,the ore - control structures are interlayer faults, conjugate shear faults, and shear faults and the genesis of these gold deposits is related to geothermal brine.
出处
《湖北地质》
1996年第2期76-80,61,共6页
关键词
泗峡口
金矿
微细浸染型
南羊山组
热卤水
Sixiakou gold deposit micro - disseminated Nanyangshan Formation geothermal brine
