文章摘要
耿同升,路小丽,罗清威,权成,秦德雨,袁要伟.坦桑尼亚PL10451矿区绿岩带型金矿床地质特征及找矿标志[J].矿产勘查,2024,15(1):73-81
坦桑尼亚PL10451矿区绿岩带型金矿床地质特征及找矿标志
Geological characteristics and prospecting signs of greenstone belt type gold deposit of PL10451 area mining in Tanzania
投稿时间:2022-10-13  修订日期:2023-11-14
DOI:10.20008/j.kckc.202401007
中文关键词: 恩泽加绿岩带  地质特征  找矿标志  坦桑尼亚
英文关键词: Nzega greenstone belt  geological characteristics  prospecting signs  Tanzania
基金项目:本文受河南省国土资源厅2017年省财政地质勘查基金项目(201710)资助。
作者单位邮编
耿同升 河南省有色金属地质矿产局第七地质大队河南 郑州450016
河南省第七地质大队有限公司河南 郑州450016 
450016
路小丽* 河南省地质矿产勘查开发局第五地质勘查院河南 郑州 450001 450001
罗清威 河南省有色金属地质矿产局第七地质大队河南 郑州450016
河南省第七地质大队有限公司河南 郑州450016 
450016
权成 河南省有色金属地质矿产局第七地质大队河南 郑州450016
河南省第七地质大队有限公司河南 郑州450016 
450016
秦德雨 河南省有色金属地质矿产局第七地质大队河南 郑州450016
河南省第七地质大队有限公司河南 郑州450016 
450016
袁要伟 河南省有色金属地质矿产局第七地质大队河南 郑州450016
河南省第七地质大队有限公司河南 郑州450016 
450016
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中文摘要:
      PL10451矿区位于坦桑尼亚环维多利亚湖南部的恩泽加绿岩带上,该绿岩带具有优越的金成矿地质条件和巨大的金成矿潜力,目前已发现有众多特大型、大型金矿床。该地区的绿岩带型金矿床类型主要包括构造蚀变岩型、石英脉型及BIF型金矿床,其成矿受构造、岩浆岩与地层等条件严格控制。本文以恩泽加绿岩带西北部的PL10451矿区为研究区,通过详细的野外地质调查和工程验证,认为矿区金矿(化)体为受剪切带控制的构造蚀变岩型金矿,矿石结构以粒状变晶结构、交代结构和碎裂结构等为主;矿石构造以稀疏浸染状构造、细脉状构造及星点状构造等为主。矿(化)体围岩蚀变特征明显,黄铁矿化、硅化、绿泥石化与该区金成矿关系密切,并具有“低阻-高极化”的地球物理特征和“Au-As明显富集”的地球化学特征。
英文摘要:
      The PL10451 mining area is located on the Nzega greenstone belt in the southern part of Lake Victoria, Tanzania. The greenstone belt has excellent gold metallogenic geological conditions and huge gold metallogenic potential. At present, many large and medium-sized gold deposits have been discovered. The main types of gold deposits in this area include structural altered rock type gold deposits, quartz vein type gold deposits and BIF type gold deposits. Its mineralization is strictly controlled by structural, magmatic rock and stratigraphic conditions.In this paper, the PL10451 mining area in the northwest of the Nzega greenstone belt is taken as the research area. Through detailed field geological investigation and engineering verification, it is considered that the gold ore (mineralization) body in the mining area is a tectonic altered rock type gold deposit controlled by the shear zone.The ore textures are mainly composed of granular crystalloblastic texture, replacement texture and cataclastic texture, and the ore structures are mainly sparse disseminated structure, veinlet structure and starlike structure. The wall rock alteration of ore body is obvious. The pyrite mineralization, silicification and chloritization are closely related to gold mineralization in this area, and which has the geophysical characteristics of “low resistivity-high polarization ” and the geochemical characteristics of “ obvious enrichment of Au-As ”.
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