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Structural setting of the Koum sedimentary basin (north Cameroon) derived from EGM2008 gravity field interpretation

机译:Koum沉积盆地(北喀麦隆)的结构设置源自EGM2008重力场解释

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摘要

This study is a contribution to the planning of hydrocarbon exploration program of the Koum sedimentary basin in North Cameroon. 3D modeling of WGM2012 gravity data derived from EGM2008 geopotential model in the Koum basin was used together with existing geological and spectral analysis information to give structural picture of the basin. The 3D model of the Koum basin confirms that the basin is developed as a half graben bounded by sub-vertical faults. The thickness of the Cenozoic sediments is about 1.5 km in the eastern part and reaches 4.5 km in the western part of the basin. Gravity lineaments computed by multi-scale analysis revealed structural trends in the E–W, NW–SE, NE–WS and N–S directions. The faults in the sedimentary terrain reach 6 km depth and have a predominant NW–SE trend with E–W trending faults along the contact between the sedimentary section and the basement complex in the northern edge.
机译:本研究是对北喀麦隆Koum沉积物盆地的油气勘探计划的贡献。 3D建模WGM2012重力数据从Koum盆地中的EGM2008 Geopotential模型衍生,与现有的地质和光谱分析信息一起使用,以提供盆地的结构图像。 Koum盆地的3D模型证实了盆地被开发为由亚垂直故障界定的半抓起来。新生代沉积物的厚度在东部约1.5公里,在盆地的西部达到4.5公里。通过多尺度分析计算的重力线路揭示了E-W,NW-SE,NE-WS和N-S方向的结构趋势。沉积地形中的故障达到6公里深度,并具有沿着沉积截面和北部边缘的地下室复合物之间的接触的E-W趋势故障具有优势NW-SE趋势。

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