塞内加尔东部下元古代复合体的结构研究

M. Ritz , A. Dia , M.F.K. Niang
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引用次数: 1

摘要

在塞内加尔东部Kedougou河早元古代地层的tonkouto - lsamuba地区沿7公里剖面的14个地点进行了大地电磁(AMT)测深。这项研究的目的是获得关于灰鲭超群的电学特性的信息。结果以视电阻率伪剖面的形式显示,表明在所有地点记录的正交分量具有明显的各向异性。因此,需要二维(2-D)建模来建立主要地质单元的电性特征。模拟结果表明,早元古代单元的电阻率范围为20,000 - 100,000 Ωm,延伸至深度为18 km。一个电阻率为1000 Ωm的主要不连续面可能是由与Kakadian基的东南边界有关的结构变化引起的。在高阻地层下,探测到电阻率急剧下降,这可能部分是由于被困流体的存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Etude structurale par la méthode audiomagnétotellurique des complexes du Protérozoïque inférieur au Sénégal oriental

Audiomagnetotelluric (AMT) soundings have been made at 14 sites along a 7 km profile in the Tonkouto-Léoba area across Early Proterozoic formations of the Kedougou Inlier in Eastern Senegal. The purpose of the study was to gain information about the electrical properties of the Mako Supergroup. The results, shown in the form of apparent resistivity pseudosections, indicate marked anisotropies for orthogonal components recorded at all sites. Consequently, two-dimensional (2-D) modelling is required to establish the electrical characteristics of the major geological units. The modelling results indicate resistivities in the range 20 000– 100 000 Ωm for the Early Proterozoic units which extend to depths of 18 km. A major discontinuity characterized by a resistivity of 1000 Ωm may arise from a structural change associated with the southeastern boundary of the Kakadian batholith. Beneath the highly resistive formations, a sharp fall of resistivity has been detected, which may be due in part to the presence of trapped fluids.

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