Basement Depth Estimation Using Euler Deconvolution and Source Parameter Imaging; a Case Study of Northeastern Part of Sokoto Basin, Nigeria

I. Abubakar, S BondeD., Y Raboh
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Abstract

Euler deconvolution and Source Parameter Imaging (SPI) geophysical interpretation techniques using Oasis Montaj version 6.4 was applied to estimate basement depth of northeastern part of Sokoto basin, northwestern Nigeria. The study area lies between longitudes of 505"E to 605"E and latitude 1205"N to 1305"N. The results of the studies indicate an increase in sedimentation northwards, with several depressions on the basement rock. The Euler deconvolution results shows the maximum depth in the study area to be 2.39 km, while Source parameter imaging indicates 1.79 km to be the highest depth. The areas where higher sedimentary thickness are observed such as sheet 11 (Rabah) and sheet 12 (Isah), are the most prospect sites where threshold temperatures could be attained.
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基于欧拉反褶积和源参数成像的基底深度估计以尼日利亚索科托盆地东北部为例
应用Oasis Montaj version 6.4欧拉反褶积和源参数成像(SPI)地球物理解释技术对尼日利亚西北部Sokoto盆地东北部基底深度进行了估算。研究区位于东经505′~ 605′、北纬1205′~ 1305′之间。研究结果表明,沉积向北增加,基底岩上有几个凹陷。欧拉反褶积结果显示研究区最大深度为2.39 km, Source参数成像显示最大深度为1.79 km。在沉积厚度较高的区域,如11层(Rabah)和12层(Isah),是最有希望达到阈值温度的地点。
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