Abdallah Atef, Adel A. Surour, Ahmed A. Madani, Mokhles K. Azer
{"title":"埃及东北部沙漠南Gabal Um Monqul和Gabal Al Kharaza远景区部分古代矿山金铜资源","authors":"Abdallah Atef, Adel A. Surour, Ahmed A. Madani, Mokhles K. Azer","doi":"10.3390/geosciences13090283","DOIUrl":null,"url":null,"abstract":"Since Antiquity, sustainable resources of gold and copper have been mined at two prominent prospects in the north Eastern Desert of Egypt, namely the south Gabel Um Monqul (SGUM) and Gabal Al Kharaza (GKZ). Mineralization is hosted by Neoproterozoic shield rocks represented by dacite and monzo- to syenogranite at the SGUM prospect whereas they are diorite, granodiorite, and quartz feldspar porphyry at the GKZ prospect. These hosts have been emplaced in an island arc environment from calc-alkaline magmas with a peraluminous to metaluminous signature. They are hydrothermally altered including albitization, sericitization, silicification, epidotization, and chloritization. The Au and Cu mineralizations are confined to shear zones that lately filled with auriferous quartz veins adjacent to mineralized alteration zones. In the GKZ prospect, the old trenches trend mainly in a NW–SE direction whereas it is NE–SW and NW–SE in the SGUM prospect. Evidence of shearing ranges from megascopic conjugate fractures and shear planes in the outcrops to microscopic sheared and crumbled Au-Cu ore assemblages dominated by Fe-Cu sulfides, specularite, and barite. Microscopic investigation suggests that the formation of specularite is due to the shearing of early existing magnetite. The ore textures and paragenetic sequence indicate that pyrite in the alteration zones is oxidized, leading to the liberation of gold up to 3.3 g/t. The formulae of the analyzed electrum lie in the range Au74.5-76.8 Ag22.2-24.5. Integration of the field, geochemistry, and mineral chemistry data, combined with the gold fire assay data prove the presence of sustainable amounts of disseminated Au and Cu, not only in the mineralized quartz veins, but also in the alteration zones. Data materialized in our paper show similarities in the style of mineralization at the SGUM and the GKZ prospects with iron oxide-copper-gold (IOCG) deposits elsewhere in the Arabian-Nubian Shield (ANS) and other world examples.","PeriodicalId":38189,"journal":{"name":"Geosciences (Switzerland)","volume":"5 1","pages":"0"},"PeriodicalIF":2.4000,"publicationDate":"2023-09-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Au-Cu Resources in Some Mines from Antiquity in the South Gabal Um Monqul and Gabal Al Kharaza Prospects, North Eastern Desert, Egypt\",\"authors\":\"Abdallah Atef, Adel A. Surour, Ahmed A. Madani, Mokhles K. 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引用次数: 0
摘要
自古以来,在埃及东北部沙漠的两个突出前景,即南Gabel Um Monqul (SGUM)和Gabal Al Kharaza (GKZ),已经开采了可持续的金和铜资源。SGUM远景区以英安岩和二长-正长花岗岩为代表的新元古代盾构岩成矿,GKZ远景区以闪长岩、花岗闪长岩和石英长石斑岩为代表。这些寄主位于具有过铝质-铝质特征的钙碱性岩浆的岛弧环境中。它们被水热蚀变,包括钠长石化、绢云母化、硅化、绿帘石化和绿泥化。金矿化和铜矿化局限于矿化蚀变带附近的剪切带,这些剪切带最近充满了含金石英脉。在GKZ远景中,古海沟主要向北西-东南方向移动,而在SGUM远景中,古海沟主要向北东-西南和北西-东南方向移动。从露头的宏观共轭断裂和剪切面到微观剪切和破碎的以Fe-Cu硫化物、镜铁矿和重晶石为主的金铜矿组合,均存在剪切作用。显微研究表明镜铁矿的形成是由于早期存在的磁铁矿的剪切作用。矿石结构和共生序列表明,蚀变带黄铁矿被氧化,导致金析出量达3.3 g/t。所分析的电极的分子式在au74.5 ~ 76.8 ag22.2 ~ 24.5范围内。综合野外、地球化学和矿物化学资料,结合金火分析资料,证明在矿化石英脉中,以及蚀变带中均存在一定量的浸染金和铜。本文中物化的数据表明,SGUM和GKZ的矿化风格与阿拉伯-努比亚盾(ANS)其他地方的氧化铁-铜-金(IOCG)矿床和其他世界例子相似。
Au-Cu Resources in Some Mines from Antiquity in the South Gabal Um Monqul and Gabal Al Kharaza Prospects, North Eastern Desert, Egypt
Since Antiquity, sustainable resources of gold and copper have been mined at two prominent prospects in the north Eastern Desert of Egypt, namely the south Gabel Um Monqul (SGUM) and Gabal Al Kharaza (GKZ). Mineralization is hosted by Neoproterozoic shield rocks represented by dacite and monzo- to syenogranite at the SGUM prospect whereas they are diorite, granodiorite, and quartz feldspar porphyry at the GKZ prospect. These hosts have been emplaced in an island arc environment from calc-alkaline magmas with a peraluminous to metaluminous signature. They are hydrothermally altered including albitization, sericitization, silicification, epidotization, and chloritization. The Au and Cu mineralizations are confined to shear zones that lately filled with auriferous quartz veins adjacent to mineralized alteration zones. In the GKZ prospect, the old trenches trend mainly in a NW–SE direction whereas it is NE–SW and NW–SE in the SGUM prospect. Evidence of shearing ranges from megascopic conjugate fractures and shear planes in the outcrops to microscopic sheared and crumbled Au-Cu ore assemblages dominated by Fe-Cu sulfides, specularite, and barite. Microscopic investigation suggests that the formation of specularite is due to the shearing of early existing magnetite. The ore textures and paragenetic sequence indicate that pyrite in the alteration zones is oxidized, leading to the liberation of gold up to 3.3 g/t. The formulae of the analyzed electrum lie in the range Au74.5-76.8 Ag22.2-24.5. Integration of the field, geochemistry, and mineral chemistry data, combined with the gold fire assay data prove the presence of sustainable amounts of disseminated Au and Cu, not only in the mineralized quartz veins, but also in the alteration zones. Data materialized in our paper show similarities in the style of mineralization at the SGUM and the GKZ prospects with iron oxide-copper-gold (IOCG) deposits elsewhere in the Arabian-Nubian Shield (ANS) and other world examples.