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甘肃马鬃山金矿成矿地质特征分析

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甘肃马鬃山金矿区位于西北地区金矿带内,其成矿地质特征具有明显的区域性和独特性.通过对该矿区地层岩性、区域构造、矿体地质特征、成矿热液活动,以及成矿物质来源等关键地质信息的系统分析与研究,揭示了马鬃山金矿的成矿地质背景与成矿机制.研究表明,该矿区金矿化主要受控于区域深大断裂系统,矿体呈脉状分布,与热液活动密切相关.成矿物质主要来源于深部岩浆热液,其成矿过程与区域构造活动及古老岩浆事件密切相关.通过对成矿模式和成矿过程的探讨,为该类金矿的勘探提供了重要理论指导.
Analysis of Metallogenic Geological Characteristics of Mazongshan Gold Mine in Gansu Province
The Mazongshan gold deposit in Gansu Province is located within the northwest gold deposit belt,and its ore-forming geological characteristics have obvious regional and unique characteristics.Through systematic analysis and research on key geological information such as stratigraphic lithology,regional structure,geological characteristics of ore bodies,hydrothermal activity of mineralization,and sources of mineralization materials in the mining area,the geological background and mechanism of mineralization in the Mazongshan gold deposit have been revealed.Research has shown that the gold mineralization in the mining area is mainly controlled by the regional deep fault system,and the ore bodies are distributed in a vein like manner,closely related to hydrothermal activity.The ore-forming materials mainly come from deep magmatic hydrothermal fluids,and their mineralization process is closely related to regional tectonic activities and ancient magmatic events.The exploration of mineralization models and processes provides important theoretical guidance for the exploration of this type of gold deposit.

mazong mountaingeological characteristics of mineralizationhydrothermal activitygold mine

吴宇杰

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甘肃省有色金属地质勘查局天水矿产勘查院,甘肃 天水 741020

马鬃山 成矿地质特征 热液活动 金矿

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(4)
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