An analysis of the genesis of this doposit was also made based on its stratigraphy, structure, meta-morphism and igneous activity, thus the metallogenetic model was astabli shed.

• 本文对四道沟金矿的区域地质、矿区地质及矿床地质特征做了论述,从地层、构造、变质及火成活动等方面对矿床的成因做了分析,并以此建立了成矿模式。