首页> 外文期刊>Arabian journal of geosciences >Exploration of new gold occurrences in the alteration zones at the Barramiya District, Central Eastern Desert of Egypt using ASTER data and geological studies
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Exploration of new gold occurrences in the alteration zones at the Barramiya District, Central Eastern Desert of Egypt using ASTER data and geological studies

机译:利用ASTER数据和地质研究在埃及中东部沙漠Barramiya地区蚀变带中发现新的金矿

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The use of ASTER data and fieldwork supported by mineralogical and geochemical analyses enabled exploration of new gold occurrences in the alteration zones in the ultramafic–mafic successions at the Barramiya district. Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) band ratios (4/8, 4/2 and 8/9 in R, G and B channels, respectively) helped in recognising of two listwaenite alteration zones (areas 1 and 2) promising for gold in the north-east and south-east of the Barramiya gold mine. Mineralogical studies and X-ray diffraction analysis revealed that areas 1 and 2 are characterized by variable concentrations of talc, ankerite, magnesite, quartz and calcite. Ore microscope studies revealed the sulphide minerals carry gold within these alteration zones; moreover, goethite and malachite are also observed. Fire assay results show Au contents in the range of 5.04 ppm in the graphite schist, 4.02 ppm in the quartz veins and 3.76 ppm in the listwaenite alteration. The atomic absorption analysis (AAS) of samples from area 1 yields an average Au content in the quartz-veins of 2.4 ppm, Ag content is 8.0 ppm and Cu content is 2.4 wt%. The listwaenite alteration gives an average Au content of 4.4 ppm and a Cu content of 2.8 wt%. In area 2, the AAS of the quartz-veins revealed an average Au content of 2.6 ppm, 6.2 ppm Ag and 1.9 wt% Cu. The listwaenite alterations of area 2 grade 3.5 ppm Au and 2.4 wt% of Cu. The Barramiya District is made up of ophiolitic ultramafic belts of serpentinites, talc carbonates and talc graphite schists, mainly thrust over the metavolcanic sequences. They include highly strained and tectonised parts enriched in sulphides, iron oxides and carbonates, with developed listwaenite alterations along the thrust contacts. Gabbro and granitic intrusions were intruded in the ultramafics and metavolcanic rocks. ASTER data are an accurate and helpful tool for detecting and mapping alteration zones for gold exploration.
机译:利用ASTER数据和由矿物学和地球化学分析支持的野外工作,可以探寻Barramiya地区超镁铁质-镁铁质演替带蚀变带中新的金矿。先进的星载热发射和反射辐射计(ASTER)的带比(分别在R,G和B通道中分别为4 / 8、4 / 2和8/9)有助于识别两个有望实现的白云母蚀变区(区域1和2)。 Barramiya金矿的东北和东南部的黄金。矿物学研究和X射线衍射分析表明,区域1和2的特征是滑石,铁矾石,菱镁矿,石英和方解石的浓度可变。矿石显微镜研究表明,硫化物矿物在这些蚀变带中携带金;此外,还观察到针铁矿和孔雀石。燃烧试验结果表明,石墨片岩中的Au含量在5.04 ppm的范围内,石英脉中的Au含量在4.02 ppm的范围内,并且在白云母蚀变中的含量为3.76 ppm。来自区域1的样品的原子吸收分析(AAS)得出,石英脉中的平均Au含量为2.4 ppm,Ag含量为8.0 ppm,Cu含量为2.4 wt%。变白钨矿的平均Au含量为4.4ppm,Cu含量为2.8wt%。在区域2中,石英脉的AAS显示平均Au含量为2.6 ppm,Ag为6.2 ppm和Cu为1.9 wt%。面积2级3.5 ppm的金和2.4 wt%的铜的方铁矿蚀变。 Barramiya区由蛇纹石,滑石碳酸盐和滑石石墨片岩的蛇绿质超镁铁质带组成,主要作用在中火山岩层上。它们包括富含硫化物,氧化铁和碳酸盐的高度应变和构造化的零件,沿推力触头发育了变白硅石蚀变。 Gabbro和花岗岩侵入体被侵入超基性岩和超火山岩中。 ASTER数据是检测和映射金矿勘探蚀变区的准确而有用的工具。

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