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Geochemical and pathfinder elements assessment in some mineralised regolith profiles in Bole-Nangodi gold belt in north-eastern Ghana

机译:加纳东北部的博乐-南迪地金带某些矿化的重生岩剖面中的地球化学和探路元素评估

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This study presents gold mineralisation and pathfinder elements characteristics in five surficial regolith profiles, with the aim of enhancing exploration strategies in the north-eastern Bole-Nangodi Gold Belt in Ghana. Samples were collected from mature soils and bedrocks in exploration pits and prepared for chemical and soil particle size analysis. 13 major elements, mineral forms and fifty-one trace elements were analysed using XRF, XRD and ICP-MS devices, respectively. SiO2, Fe2O3-MnO and Al2O3 are elevated in the A, B and C horizons, respectively, while Na2O-K2O-MgO-CaO-P2O5 systems dominate the bedrocks. Gold pathfinder element suites of As-Mo-Ag-Sn-Sb-Te-W-Hg-Bi are above Primitive Mantle values by a factor of5, while the mean chemical index of alteration (CIA) values are above 80%. Profiles contain70% quartz with stable mineral concentrations of 53, 18 and 29% in the A, B and C, horizons, respectively. The B horizon is the most altered horizonbased on CIA, loss on ignition and Fe/Al ratios; the horizon accounts for 52% of the material and 76% of elements in the2mm particle size. Mass balance and principal component analysis shows that Au exploration targets and the associated pathfinder element suites are the following: (1) horizon A with Sr-Ca-Ge-Sn-Th in the amphibolite and biotite gneiss profiles (2) horizons A and B with S-K-Zr-Tl-Ge in the volcaniclastic and (3) the bedrocks with Cu-Pb-Sb-Ag-Mo and Mn-Cr-Ba-V-Ce-Bi-Fe-Co-Sb-As-Se of the metavolcanic and phyllite profiles, respectively. The regolith models summarise the mineralogical and structural framework of the profiles and may largely influence exploration designs.
机译:这项研究介绍了五个表面重生石剖面中的金矿化和探路元素元素特征,目的是增强加纳东北部的博乐-南戈迪金矿带的勘探策略。在勘探坑中从成熟的土壤和基岩中收集样品,并准备进行化学和土壤粒度分析。使用XRF,XRD和ICP-MS装置分别分析了13种主要元素,矿物形态和51种微量元素。 SiO2,Fe2O3-MnO和Al2O3分别在A,B和C层中升高,而Na2O-K2O-MgO-CaO-P2O5系统主导基岩。 As-Mo-Ag-Sn-Sb-Te-W-Hg-Bi的金探路者元素套件比原始地幔值高> 5,而平均化学变化指数(CIA)值则在80%以上。剖面包含> 70%的石英,A,B和C层中的稳定矿物质浓度分别为53、18和29%。基于CIA,点火损失和Fe / Al比,B层是变化最大的层。在大于2mm的粒径中,地平线占材料的52%,元素占76%。质量平衡和主成分分析表明,Au勘探目标和相关的探路者元素套件如下:(1)在角闪岩和黑云母片麻岩剖面中具有Sr-Ca-Ge-Sn-Th的层位A(2)层位A和B (3)基岩中含有Cu-Pb-Sb-Ag-Mo和Mn-Cr-Ba-V-Ce-Bi-Fe-Co-Sb-As-Se分别是变火山岩和千枚岩剖面。 go石模型总结了剖面的矿物学和结构框架,并可能在很大程度上影响勘探设计。

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