METAMORPHISM AND DEFORMATION OF GOLD-BEARING NEOPROTEROZOIC WONAKA SCHIST BELT, NORTHWEST-NIGERIA.

U. S. Umar
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Abstract

The role of metamorphism and deformation is indispensable in the occurrences of gold mineralization worldwide. In this work, deformation and metamorphic conditions for gold-bearing Neoproterozoic Wonaka Schist Belt; located around Kutcheri town of Tsafe Local Government of Zamfara State, was investigated. This is achieved using metamorphic litho-minerals obtained from ternary plots via X-Ray fluorescence (XRF) geochemical data, and directly using minerals phases from X-Ray Diffraction (XRD) technique. Index minerals identified from petrographic analysis previously suggest low to medium-grade metamorphism (M1). XRD analysis indicates quartz, albite, oligoclase, microcline, chlorite, and biotite, suggesting greenschist to lower amphibolite facies (M2). Sillimanite, andalusite, kyanite, staurolite, chlorite, biotite, and garnet were identified from the ternary plots using XRF major oxides, indicating upper amphibolite to granulite facies metamorphism (M3). This is typical of prograde metamorphism, granulite facie metamorphic grade is indicated. Na2O/Al2O3 versus K2O/Al2O3 for petrogenetic character suggests shale provenance, while the trace elements spider diagram indicates Wonaka litho-units as co-genetic compositionally, as high concentrations of V and Cr linked the petrogenetic affinity to mafic sources. Three circles of deformations are indicated; ductile deformation (D1) of the paleosome Schist producing foliations and lineation, brittle type (D2) in mid Pan-African and was accompanied by several fractures and felsic intrusions. Late Pan-African (D3) involves the folding of banded orthogneisses, the development of boudinage as well as intense shearing (ductile fault). Geospatial analysis of the fractures suggests that they represent regional Pan-African sutures cross-cutting Nigeria into the Atlantic and up to South American plate. The research therefore concludes that Au-fluid emanating through this regional event, utilizes D2 as channel ways and loci. D3 with M3 engulfed the entire structures repositioning the geometry to its present disposition.
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尼日利亚西北部新新生代含金温纳卡片岩带的变质作用和变形。
变质和变形在全球金矿成矿过程中发挥着不可或缺的作用。在这项研究中,对位于赞法拉州 Tsafe 地方政府 Kutcheri 镇周围的新新生代 Wonaka 片岩含金带的变形和变质条件进行了调查。研究使用了通过 X 射线荧光 (XRF) 地球化学数据从三元图中获得的变质岩矿物,以及直接使用 X 射线衍射 (XRD) 技术获得的矿物相。之前通过岩相分析确定的指数矿物表明存在中低级变质作用(M1)。X 射线衍射(XRD)分析表明有石英、白云石、低斜长石、微绿泥石、绿泥石和斜长石,表明为绿帘石至低闪长岩面(M2)。利用 X 射线荧光主要氧化物从三元图中确定了矽线石、安达拉石、黝帘石、白云石、绿泥石、斜长石和石榴石,表明是上闪长岩至花岗岩面变质作用(M3)。这是典型的顺级变质作用,表明花岗岩面变质等级。Na2O/Al2O3与K2O/Al2O3的岩石成因特征表明了页岩的来源,而微量元素蛛网图则表明沃纳卡岩性单元在成分上是共成因的,因为高浓度的V和Cr将岩石成因亲和力与黑云母来源联系在一起。图中标出了三个变形圈;古岩体片岩的韧性变形(D1)产生了叶状和线状变形,泛非中期的脆性变形(D2)伴随着几条断裂和长岩侵入体。泛非晚期(D3)涉及带状正长片麻岩的褶皱、拗陷的发育以及强烈的剪切(韧性断层)。对断裂的地理空间分析表明,这些断裂代表了横切尼日利亚到大西洋、直至南美洲板块的泛非区域缝合线。因此,研究得出结论,通过这一区域性事件涌出的金流体利用 D2 作为通道和地点。D3 和 M3 吞没了整个结构,将几何形状重新定位到目前的位置。
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