喀麦隆沿海地区Pouma中部石英岩矿床的岩石学、形态构造和地球物理研究

Paho Nteinmusi Jude , Kenfack Jean Victor , Wotchoko Pierre , Njoh Olivier Anoh , Makem Elvise Abasoh , Demanou Messe Malick Rosvelt , Tabod Charles Tabod
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引用次数: 1

摘要

为了确定Pouma-Cameroon石英岩矿床沿douala - yaound轴的横向延伸范围,对其进行特征描述,除其他事项外,还需要检查岩石学和形态结构领域,并确定研究地区地层的电性。使用斯伦贝谢式电极配置进行了24个垂直电测深点;另外,还进行了7个手动螺旋钻钻孔,形成了KH、QH、AKH、H、HK、AK、HA、A等曲线类型;而岩性测井则以粘土砂质为质地,由细粒粘土砂质变为红土质。密度的计算以及岩石构造的研究使得确定研究区域的地质背景成为可能。所获得的各种结果使我们能够在研究区域的中心定位新鲜的石英岩地层。它沿着douala - yaound轴延伸超过1871.4米的新地层和1991米的稍微改变的地层。
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Petrographic, morpho-structural and geophysical study of the quartzite deposit in the central part of Pouma, Littoral-Cameroon

The characterization of the Pouma-Cameroon quartzite deposit with the aim of determining its lateral extension along the Douala-Yaoundé axis required, among other things, the examination of the petrographic and morpho-structural domain as well as the determination of the electrical properties of the formations in the study area. 24 vertical electrical sounding points were carried out using a Schlumberger type electrode configuration; also, 7 manual auger boreholes were carried out, these resulted on one hand in the following types of curves: KH, QH, AKH, H, HK, AK, HA, A; and on the other hand to lithological logs with a clayey sandy texture, gravelly clayey sand to lateritic. The calculation of the densities as well as the petro-structural studies made it possible to confirm the geological context of the study area. The various results obtained permitted us to locate the fresh quartzite formation at the center of the study area. It stretches along the Douala-Yaoundé axis over 1871.4 m for the fresh formation and 1991 m for the slightly altered formation.

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