用磁性方法估算尼日利亚阿达马瓦槽部分地区沉积厚度的油气潜力

Ajala S.A, Salako K. A, Rafiu A. A, Alahassan U. D, A. T, Sanusi Y.A
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引用次数: 0

摘要

本研究介绍了阿达马瓦槽部分地区航磁数据的分析和解释结果,目的是调查研究区的油气潜力。研究区位于北纬8.50°至9.50°,东经11.50°至12.50°之间。研究区的总磁场强度图经过了区域/残差分离。在残差图上应用三种深度估计技术来确定研究区沉积物的厚度:源参数成像、欧拉反褶积和光谱法。这些方法的结果证实:;SPI、Euler反褶积和光谱法显示,研究区东北部的厚沉积分别为4.42km、4.20km和4.17km。SPI、Euler反褶积和谱法分别揭示了研究区东南部、南部和西南部0.06km、0.10km和0.42km的浅层深度。本研究中在研究区域东北部(对应于Numal)获得的超过4km的最大沉积厚度可能足以使碳氢化合物成熟和聚集。研究区具有良好的油气勘探前景。
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ESTIMATION OF SEDIMENTARY THICKNESS FOR HYDROCARBON POTENTIAL OVER PART OF ADAMAWA TROUGH, NE NIGERIA USING MAGNETIC METHOD
This study presents the results of the analysis and interpretation of aeromagnetic data over part of Adamawa trough with the aim of investigating the hydrocarbon potential of the study area. The study area is located between latitude 8.50oN and 9.50oN and longitudes 11.50oE and 12.50oE. The Total magnetic intensity map of the study area was subjected to regional/residual separation. Three depth estimating techniques applied on the residual map to determine the thickness of sediments in the study area were Source parameter imaging, Euler deconvolution and spectral method. The results of these methods corroborate; the SPI, Euler Deconvolution and Spectral method shows a thick sedimentation of 4.42 km, 4.20 km and 4.17 km at the north-eastern part of the study area respectively. The SPI, Euler deconvolution and the Spectral method reveal shallow depth of 0.06 km, 0.10 km and 0.42 km at the southeast, southern and southwest part of the study area respectively. The maximum sedimentary thickness of above 4 km obtained in this study at the north-eastern part of the study area which corresponds to Numal might be sufficient for hydrocarbon maturation and accumulation. The study area was found to have a good prospect for hydrocarbon exploration.
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