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首页> 外文期刊>Journal of Earth Sciences and Geotechnical Engineering >Imaging the Subsurface in the Cameroon Centre Region using the Audio-magnetotellurics (AMT) Soundings forthe Monitoring of the Monatele-sa’a Earthquake Area
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Imaging the Subsurface in the Cameroon Centre Region using the Audio-magnetotellurics (AMT) Soundings forthe Monitoring of the Monatele-sa’a Earthquake Area

机译:使用音频大地电磁(AMT)测深对喀麦隆中心地区的地下影像进行成像,以监测Monatele-sa’地震区

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摘要

In monitoring the Monatélé-Sa’a earthquake area, audiomagnetotelluric investigation was carried out using a scalar instrument with a frequency range from 4.1 Hz to 2300 Hz. Data have been collected in the Ntui-Sa’a area near Monatélé, along a profile containing seven (07) stations directed N-S, covering approximately a distance of 16.5 km. This profile crosses the Sanaga River which seems to be parallel to a buried big fault which shows no indication on the surface. The validation of the measured resistivity and calculated phase data set is done by the application of dimensionality. The interpretation of data using 2D inversion imaging of the subsurface has lead to the confirmation of two major discontinuities: ? The Sanaga fault oriented SSW-NNE, covered by a thick layer of alluvial deposit in the Elang III area. This fault is bisected to a lateral fracture between Nkolessono and Elang III.
机译:在监视Monatélé-Sa’a地震区时,使用频率范围为4.1 Hz到2300 Hz的标量仪器进行了电磁观测。数据已经在Monatélé附近的Ntui-Sa’a地区收集,沿一个包含指向N-S的七(07)个台站的概况,覆盖了大约16.5 km的距离。该剖面穿过萨那加河,该河似乎与一个埋没的大断层平行,在断层上未显示任何迹象。测得的电阻率和计算出的相位数据集的验证是通过应用维数进行的。使用地下2D反演成像对数据的解释导致了两个主要不连续性的确认: Sanaga断层为SSW-NNE,在Elang III地区被厚厚的冲积层覆盖。该断层被一分为二,在恩科勒索诺(Nkolessono)和依兰三世(Elang III)之间发生横向裂缝。

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