Geophysical Signature Location in the South-West of Chad: Structural Implications

Diponbe Benoit, N. Robert, Kenfack Jean Victor, Momo Tonfack Christian
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引用次数: 2

Abstract

A study is conducted in South-West of Chad with the goal of underlining the different lineaments of the region, which are entirely or partially hidden by the sedimentary cover. Different gravity data processing techniques including horizontal gradient of vertical derivative coupled with upward continuation and Euler’s de-convolution are used. These methods revealed a number of lineaments describing gravity density discontinuities whose directions are N-S, NE-SW, ENE-WSW, and WNW-ESE at NNW-SSE. However, the predominant direction for major lineaments is WNW-ESE. The major lineaments associated to the faults are: F1, F2, F3, F6, F7, F8, F9, F10, F14, F21, F22, F23, F24 and F28. Euler’s solutions indicate depths up to 9.2 km for the anomaly sources. Such lineaments are very useful for groundwater and oil exploration, but also for risk assessment.
乍得西南部地球物理特征位置:构造意义
在乍得西南部进行了一项研究,目的是突出该地区完全或部分被沉积盖层掩盖的不同地貌。不同的重力数据处理技术,包括水平梯度垂直导数耦合向上延拓和欧拉反卷积。这些方法揭示了NNW-SSE上的N-S、NE-SW、ENE-WSW和WNW-ESE方向的重力密度不连续特征。然而,主要地貌的主导方向是WNW-ESE。与断裂相关的主要地貌为:F1、F2、F3、F6、F7、F8、F9、F10、F14、F21、F22、F23、F24和F28。欧拉解表明异常源的深度可达9.2 km。这种轮廓线对地下水和石油勘探非常有用,但对风险评估也很有用。
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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