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Structural and Lithological Study of Gold Mineralization in the Areas of Bena and Bakolobi, Mali, West Africa

机译:贝纳和巴克罗毕,马里,西非贝加尔邦的金矿化结构和岩性研究

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The areas of Bena-Bakolobi are located in the eastern part of the Kedougou-Kenieba in layer. This sector contains several deposits of gold, including the mines of Sadiola, complex Gara-Yalea and Gounkoto, gold mines of Tabakoto and the gold deposit of Fekola, all located around the (SMS) Senegalo Malian shear zone. The work carried out is summarized in two parts: The first part is based on the detailed mapping of the Bena and Bakolobi target. It was necessary to make a detailed mapping in order to understand and assess the target. The second part is to determine the term and the litho-structural control of gold mineralization. This study is based on lithology, alteration, structures and mineralization of the two areas. The ultimate purpose is to draw a regolith map for a future research program. Two types of alteration affect the rock formations of the two zones: weathering (supergene) that consists in hematization, limonitisation and the kaolinitization. The hydrothermal alteration consists in albitization, chloritisation, the sericitization, the tourmalinisation, the sulphidation, silicification and carbonation. This paper improves structural and lithological study of gold mineralization in the areas of Bena and Bakolobi. The analysis of the results of the work carried out in the two zones allowed us to have an overview on the geology of these two zones, which are located in the Kédougou-Kéniéba window in the volcano-sedimentary rocks of Proterozoic Formation of Kofi. The lithological and structural studies carried out in the area have demonstrated the relationship between structures and mineralization and/or lithology.
机译:Bena-Bakolobi的地区位于kedougou-kenieba的东部。该部门含有几款金矿床,包括Sadiola,Complex Gara-Yalea和Gounkoto的Mines,Tabakoto的金矿和Fekola的金矿床,所有这些都位于(SMS)Senegalo MalianShear区周围。所开展的工作总结了两部分:第一部分是基于Bena和Bakolobi目标的详细绘图。有必要进行详细的映射,以便理解和评估目标。第二部分是确定金矿化的术语和立体结构控制。本研究基于两个区域的岩性,改变,结构和矿化。最终目的是为未来的研究计划绘制一个乐高质标的地图。两种类型的改变影响了两个区域的岩层:静脉化(叠烯),其包括血化,褐发质炎和高岭化。水热改变包括脱硫,氯耳动,树苗化,林林化,亚硫化,硅化和碳酸化。本文提高了Bena和Bakolobi地区的金矿化结构和岩性研究。分析了两个地区所开展的工作结果允许我们概述这两个区域的地质,位于Kofi的前古代的火山沉积岩中的Kédougou-kéniéba窗口中。该地区开展的岩性和结构研究表明了结构和矿化和/或岩性之间的关系。

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