利用航磁数据对尼日利亚尼日尔三角洲部分地区的地下结构进行调查

M. M. M. Ekpa, J. C. Ibuot, F. Okeke, D. Obiora
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引用次数: 1

摘要

利用航磁法进行了地球物理研究,以调查尼日利亚尼日尔三角洲的部分地区,目的是调查研究区域内异常体的原因和性质。采用光谱分析技术进行定量解释,确定了区内沉积盆地深度/厚度、基底地形、构造走向、居里点深度、热梯度和热流。总磁强度(TMI)异常值在-53.7 ~ 119.5nT之间,残磁强度在-52.5 ~ 58.0nT之间。光谱分析显示,磁源深度在2.5 ~ 5.5km之间,浅层磁源深度在0.89 ~ 1.47km之间。地温分析结果表明,该地区居里点深度为11.782 ~ 18.048km,地温梯度为32.137 ~ 49.2310,其分布范围为𝑘𝑚−1。热流值范围为80.343 ~ 123.080𝑚𝑊𝑚−2。研究结果为进一步认识研究区地下构造的变化提供了新的思路。这些将加强资源的开发,如果利用得当,将为国家带来经济利益。然而,未来可能对这一活跃区域进行的研究工作被提出,以获得更可靠的结果。
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INVESTIGATION OF SUBSURFACE STRUCTURES WITHIN PARTS OF NIGER DELTA, NIGERIA, VIA AEROMAGNETIC DATA
Geophysical study involving aeromagnetic method was carried out to investigate parts of Niger Delta in Nigeria, aimed at investigating the cause and nature of anomalous bodies within the study area. Spectral analysis technique was employed in quantitative interpretation to determine depth/thickness of the sedimentary basin, basement topography, structural trends, curie point depth, thermal gradient and heat flow in the area. The total magnetic intensity (TMI) anomalies had values of between -53.7nT and 119.5nT while the residual magnetic intensity ranged from -52.5 to 58.0nT. The spectral analysis revealed the depth to magnetic sources varying from 2.5 to 5.5km while the shallow magnetic sources varied from 0.89 to 1.47km. The geothermal analysis revealed the curie point depth between 11.782 and 18.048km while the calculated geothermal gradient ranged lie between 32.137 and 49.231o𝐶𝑘𝑚−1. The heat flow values ranged from 80.343 to 123.080𝑚𝑊𝑚−2. The results from this study have thrown more light to the understanding of the variation of subsurface structures in the study area. These will enhance the development of the resources and will be of economic benefit to the country if well harnessed. However, possible future research work on this active area is proposed for more robust results.
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