| 厄立特里亚Koka金矿床成矿流体特征及其地质意义 |
| Received:July 04, 2018 Revised:September 03, 2018 点此下载全文 |
| 引用本文：ZHAO Kai,YAO HuaZhou,WANG JianXiong,XIANG WenShuai,Ghebsha Fitwi Ghebretnsae.2018.Characteristics of ore-forming fluids of Koka gold deposit in Eritrea and their geological significances[J].Mineral Deposits,37(6):1337~1348 |
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| Author Name | Affiliation | | ZHAO Kai | Wuhan Center, China Geological Survey, Wuhan 430205, Hubei, China | | YAO HuaZhou | Wuhan Center, China Geological Survey, Wuhan 430205, Hubei, China | | WANG JianXiong | Wuhan Center, China Geological Survey, Wuhan 430205, Hubei, China | | XIANG WenShuai | Wuhan Center, China Geological Survey, Wuhan 430205, Hubei, China | | Ghebsha Fitwi Ghebretnsae | College of Silk Road, China University of Geosciences, Wuhan 430074, Hubei, China |
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| 基金项目:中国地质调查局项目“埃及及邻区矿产资源潜力评价”（编号：DD20160109）项目资助 |
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| 中文摘要:厄立特里亚Koka金矿床产于努比亚地盾新元古代浅变质岩系中，矿体主要赋存于Koka微晶花岗岩内，受剪切构造控制，是在该国发现的大型造山型金矿床。矿床含金石英脉中石英中赋存的原生流体包裹体分为富CO2包裹体、CO2-H2O包裹体和H2O包裹体共3种类型，以大量发育富CO2包裹体与CO2-H2O包裹体为特征。成矿流体具有富CO2、中低温（210~360℃）、中低盐度（w（NaCleq）=2.24%~8.51%）的特征。流体中阳离子主要为Na+与少量K+，阴离子为Cl-与少量SO42-，气相成分主要为CO2与H2O，基本不含其他气体组分，流体属于NaCl-H2O-CO2体系。成矿流体密度变化范围较大（0.597~0.969 g/cm3），其中高密度的富CO2包裹体捕获的最小P-T条件为260~360℃、100~270 MPa，形成于区域变质作用时期。成矿流体的δDV-SMOW范围为-57‰~-50.1‰，δ18O水范围为1.4‰~3.2‰，表明Koka金矿床成矿流体主要来源于变质热液，并伴有大气降水的混入。成矿流体中CO2-H2O包裹体气相分数变化范围很大（15%~80%），与之共生的H2O包裹体具有相似的盐度以及较低的均一温度，表明初始的CO2-H2O型流体发生了不混溶作用，导致相分离，产生的大量富CO2流体，并使金大量沉淀。 |
| 中文关键词:地球化学 成矿流体 流体包裹体 不混溶 Koka金矿 厄立特里亚 |
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| Characteristics of ore-forming fluids of Koka gold deposit in Eritrea and their geological significances |
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| Abstract:Located in the metamorphic strata of the Nubian Shield, the Koka gold deposit is a large orogenic gold deposit in Eritrea. The orebody hosts in the Koka aplitic granite, controlled by shear structure. The primary fluid inclusions in gold-bearing quartz veins can be divided into three types, i.e., extremely CO2-rich inclusions, CO2-H2O inclusions and H2O inclusions, with CO2-rich inclusions and CO2-H2O inclusions being dominant. The oreforming fluid is characterized by rich CO2, medium-low temperature (210~360℃) and low salinity (w(NaCleq)=2.24%~8.51%). In the liquid phase components, the cations mainly include Na+ and a little K+, the anions contain Cl- and a little SO42-, the gaseous content of the fluid inclusion is primarily CO2 and secondly H2O, almost without any other gaseous content, and the fluids belong to NaCl-H2O-CO2 system. The density of ore-forming fluid has a large variation (0.597~0.969 g/cm3), and the trapping P-T conditions of CO2-rich inclusions characterized by high density can be estimated to be 260~360℃ and 100~270 MPa, usually formed in regional metamorphism period. δDV-SMOW of the fluid is between -57‰ and -50.1‰, whereas δ18OH2O of the fluid is between 1.4‰ and 3.2‰, which suggests that the source of the ore-forming fluid for Koka gold deposit came mainly from metamorphic water mixed with meteoric water. The filling degree of CO2-H2O inclusions has a large variation (15%~80%), and symbiotic H2O inclusions have similar salinities and lower uniformity temperature, indicating that the original CO2-H2O fluid experienced fluid immiscibility, which resulted in the phase separation that formed a mass of CO2-rich fluid and caused gold precipitation. |
| keywords:geochemistry ore-forming fluid fluid inclusion immiscibility Koka gold deposit Eritrea |
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