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首页> 外文期刊>Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration >Genetic implications of fluid-deposited disordered graphite and methane-rich inclusions in the Jonnagiri granodiorite-hosted gold deposit, Eastern Dharwar Craton, India
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Genetic implications of fluid-deposited disordered graphite and methane-rich inclusions in the Jonnagiri granodiorite-hosted gold deposit, Eastern Dharwar Craton, India

机译:在jonngiri granodiorite-hosted金矿床,东部Dharwar Craton,印度的遗传缺陷型石墨和富含甲烷的夹杂物的遗传影响

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Graphical abstractDisplay OmittedHighlights?Disordered graphite and CH4-rich fluid in fluid inclusions.?FluidfO2values were calculated and C-O-H phase diagram was computed.?Wide variation in fluidfO2with the fluid composition.?Gold precipitation is a result of lowfO2, during fluid-rock interaction.AbstractLaminated quartz veins, occurring within sheared granodiorite in the Jonnagiri greenstone belt, host lode gold mineralization. The greenstones were metamorphosed to lower amphibolite facies condition. Hydrothermal alteration produced inner zone of auriferous laminated quartz vein and contiguous proximal zone within the sheared granodiorite. Detailed fluid inclusion studies by Saravanan et al. (2009) reveal presence of three types of fluid inclusions. These are type-I aqueous-gaseous, type-II gaseous and type-III low saline aqueous inclusions. Raman spectroscopic studies performed in this study, on type-II inclusions in quartz veins from the inner and proximal zones reveal presence of disordered graphite, occurring as thin films within fluid inclusions, apart from variable proportions of CO2,CH4and H2O. Perple_X -aided phase diagram computations were carried out in the C-O-H system at 300°C and 2kbar to examine the chemical evolution of the C-O-H fluids. The calculated logfO2values on the graphite saturation surface range from ?35.71 to ?32.65 when XOvaries from 0.1 to 1.0. However, logfO2decreases significantly to ?49.31 at XO=0.1E–07 that pertains to the stability of almost pure CH4. Nearly similar logfO2values were reproduced from the calculations using the COH spread sheet. Decrease infO2, as demonstrated by the occurrence of gaseous fluid inclusions with disordered graphite and varying proportions of CO2-CH4in the gaseous part, played a dominant role in decreasing gold solubility during fluid-rock interaction and precipitating gold at Jonnagiri.]]>
机译:<![cdata [ 图形摘要 显示省略 突出显示 < CE:简单段ID =“SP0010”View =“全部”> 无序石墨和ch 4 -rich流体夹杂物中的液体。 < / ce:list-item> Fluid f o 2 计算值,计算COH相图。 流体的宽变化 f o 2 用流体组成。 金降水是低 F O 2 ,在流体摇滚期间互动。 抽象 < CE:简单 - 段ID =“SP0015”视图=“全部”>层压石英静脉,在Jonngiri Greenstone Belt中的剪切Granodiorite内发生,主持洛登金矿化。绿色的岩石变质到较低的倒数倒数相位。水热改变在剪切的Graniotiorite内产生了纤维叠层石英静脉和连续近端区域的内部区域。 Saravanan等人的详细流体包涵体研究。 (2009)揭示了三种类型的液体夹杂物。这些是I型水性气态,II型气态和III型低盐水含水夹杂物。在本研究中进行的拉曼光谱研究,从内部和近端区域的石英静脉中的II型夹杂物揭示了紊乱的石墨的存在,在流体夹杂物内作为薄膜发生,除了CO 2, CH 4 和H 2 O. PERPLE_X -AIFED相图计算计算在300℃和2kBAR的C-O-H系统中进行,以检查C-O-H流体的化学进化。计算的日志 f o 2 石墨饱和表面的值从?35.71到?32.65 x O 各种0.1到1.0。但是,日志 f o 2 在x o = 0.1e-07涉及几乎纯ch 4 的稳定性。几乎类似的日志 f o 2 使用COH Spread Spects从计算中再现值。 f o 2 ,如含有紊乱的石墨和不同比例的气体流体夹杂物的发生。 2 -ch 4 在气体部分,在减少金溶解度时起到了主导作用在Jonngiri的流体岩相互作用和沉淀金。 ]]>

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