利用数字化航磁数据估算尼日利亚南部-西部伊巴丹震源参数

A. A. Alabi, O. Olowofela
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引用次数: 1

摘要

从尼日利亚地质调查局获得伊巴丹地区地理纬度为7000 €ŸN至7030 €ŸN,经度为3 30 €²E至4 00 €²E的航空磁资料。对资料进行了分析,绘制了地下构造图,并对磁资料进行了定量和定性解释,推导了震源参数。利用向上延拓技术去强调短 -波长异常,利用局部波数技术确定该区磁源深度,并利用解析信号获得磁基底深度。局部波数法、向上延拓法和视磁化率法的分析,在圈定伊巴丹地区的地质构造、震源参数和磁化率等方面,显著提高了磁资料的解释水平。这些深度范围从0.607公里到2.48公里。50 m截止波长处的视磁化率图范围为-0.00012 ~ 0.00079,与部分岩石类型的磁化率值一致;花岗片麻岩,混辉岩黑云母片麻岩,黑云母白云母花岗岩,角闪石花岗岩,石英和片岩。局部波数的结果表明,在整个研究区磁基底表面沿剖面存在变化。
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ESTIMATION OF SOURCE PARAMETERS IN IBADAN, SOUTH – WESTERN NIGERIA USING DIGITIZED AEROMAGNETIC DATA
Airborne magnetic data covering geographical latitudes of 7000‟N to 7030‟N and longitudes of 3 30′E to 4 00′E within Ibadan area were obtained from Nigeria Geology Survey Agency. The data were ana-lyzed to map the sub surface structure and the source parameters were deduced from the quantitative and qualitative interpretation of magnetic data. The upward continuation technique was used to de-emphasize short – wavelength anomaly while the depth to magnetic sources in the area was deter-mined using local wavenumber technique, the analytic signal was also employed to obtain the depths of the magnetic basement. Analysis involving the local wavenumber, upward continuation and appar-ent magnetic susceptibility techniques significantly improves the interpretation of magnetic data in terms of delineating the geological structure, source parameter and magnetic susceptibility within Iba-dan area.. These depth ranges from 0.607km to 2.48km. The apparent susceptibility map at the cut-off wavelength of 50 m ranges from -0.00012 to 0.00079 which agree with the susceptibility value of some rock types; granite gneiss, migmatite biotite gneiss, biotite muscovite granite, hornblende granite, quartz and schists. The result of the local wavenumber suggests variation along the profiles in the surface of magnetic basement across the study area.
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