新疆红柳沟锰矿地质特征与成矿机理研究

Research on Hongliugou Geological Characteristics and Metallogenic Mechanism of Xinjiang Manganese Mine

新疆红柳沟矿区位于天山地槽褶皱系、北天山优地槽褶皱带觉罗塔格复背斜中的库姆塔格—白山泉褶皱束中段北侧,即雅满苏壳型大断裂中段北侧,属塔里木古板块中的伊林哈比尔尕一觉罗塔格华力西岛弧带东部。新疆红柳沟锰矿受构造控制,主要为沉积变质型锰矿。本文对矿区地层特征、构造特征、矿床地质特征进行详细分析,进而对矿区成矿机理进行深入研究,对以后的工作具有十分重要的参考意义。

The mine is located in the Tianshan Hongliugou geosyncline fold system, northern Tianshan fold belt eugeosynclinal Jueluotage anticlinorium in Kumtag - fold the north side of the beam in the middle Baishan Quan, Su-shell big break in the middle Ya Man on the north side, is the ancient Tarim plate in Elaine Habierga rota Ga Jueluotage Variscan island arc east. Hongliugou manganese controlled by the structure, mainly sedimentary metamorphic manganese. In this paper, mining stratigraphic features, structural characteristics, deposit geological features in detail, and then the mechanism of mineralization mining depth study, a reference of great significance for the future work.