首页|津巴布韦CHEGUTU GOLD金矿地质特征与找矿标志研究

津巴布韦CHEGUTU GOLD金矿地质特征与找矿标志研究

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CHEGUTU GOLD金矿围岩为太古界塞巴奎系条带状含铁硅质岩、铁镁质片岩、变质粗玄岩及蛇纹岩等,金成矿与区内NNW向韧性剪切带密切相关,矿体产状总体与区内糜棱叶理产状一致.矿石类型以石英细脉型为主.围岩蚀变有硅化、绢云母化、绿泥石化、碳酸盐化等,以硅化为主,越靠近矿体,硅化越强烈;矿体内以金属矿化为主,以黄铁矿化、黄铜矿化常见,金属硫化物与金的富集呈正相关,矿床成因类型为变质-热液型,多种找矿标志明显,研究结果为以后的地质勘查提供重要参考.
Geological characteristics and prospecting indicators of CHEGUTU GOLD gold deposit in Zimbabwe
The surrounding rock of the CHEGUTU GOLD gold deposit is a belt like iron bearing siliceous rock,iron magnesium schist,metamorphic dolomite,and serpentinite of the Archaean Sebakui series.The gold mineralization is closely related to the NNW trending ductile shear zone in the area,and the overall occurrence of the ore body is consistent with the occurrence of mylonitic foliation in the area.The ore type is mainly quartz vein type.Surrounding rock alteration includes silicification,sericitization,chloritization,carbonation,etc.,with silicification being the main type.The closer to the ore body,the stronger the silicification;The ore body is mainly composed of metal mineralization,with pyrite and brass mineralization being common.Metal sulfides are positively correlated with gold enrichment,and the genesis type of the deposit is metamorphic hydrothermal.There are multiple obvious prospecting indicators,and the research results provide important references for future geological exploration.

Zimbabwegold depositgreenstone beltore genesisprospecting criteria

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江西省地质局第八地质大队,江西 上饶 334000

津巴布韦 金矿 绿岩带 矿床成因 找矿标志

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.(15)
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