Mineralogy and Geochemistry of Eteké Eburnean Gold Deposit (Gabon)

Makarim Dalil, Nazaire Nzaou Mabika, A. Wafik, Zohir Baroudi, Abdelmalek Ouadjou, M. Gharrabi, Amine Bouwafoud, Nouamane El Aouad, Y. Zerhouni, S. Alikouss
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Abstract

The Gabon geology offered favorable and natural environments for the formation of various types of mineralization. The Etéké gold district, aim of this study, is located in the Ngounié province (southern Gabon) on the western edge of the Chaillu massif. Geologically, the gold mineralization is associated with the Eburnean orogeny and hosted in the Archean greenstone belts. Also, this deposit is covered by a significant vegetation cover and a very extensive lateritic weathering profile, which hinders the most accurate study. Through this paper, we aim to propose a genesis pattern of this mineralization via a multidisciplinary approach. To do this, a petrographic, metallogenic, and geochemical characterization has been established in the different sectors of the Etéké deposit. The studied deposits display varied facies which are encased in granitoid. They are essentially formed of abundant granitoid, and amphibolite compared to the volcano-sedimentary formations. These rocks display magmatic textures, affected by metamorphism, and not sufficiently preserved. Based on our multidisciplinary approach, the studied samples collected from the core’s boreholes allowed us to decipher a volcanogenic and metamorphosed origin of the gold genesis.
加蓬etek Eburnean金矿床的矿物学和地球化学特征
加蓬地质为各种类型矿化的形成提供了有利的自然环境。作为本研究目的的et k金矿区位于Chaillu地块西部边缘的ngouni省(加蓬南部)。地质上,金矿成矿与鄂本造山运动有关,赋存于太古宙绿岩带。此外,该矿床被显著的植被覆盖和非常广泛的红土风化剖面所覆盖,这阻碍了最准确的研究。通过本文,我们旨在通过多学科的方法提出这种成矿的成因模式。为此,在et k矿床的不同区域建立了岩石学、成矿学和地球化学特征。研究的矿床表现为花岗岩类包裹的不同相。与火山-沉积构造相比,它们主要由丰富的花岗岩和角闪岩组成。这些岩石显示岩浆结构,受变质作用的影响,没有得到充分保存。基于我们的多学科方法,从岩心钻孔中收集的研究样本使我们能够破译火山成因和变质成因。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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