Iwaraja断裂南翼系统的多技术填图

A. Anifowose, M. I. Oladapo, O. Akpan, C. Ologun, O. O. Adeoye-Oladapo, S. Y. Tsebeje, T. Yakubu
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引用次数: 15

摘要

利用遥感和地电技术对尼日利亚Ifewara-Zungeru断裂带Iwaraja段进行了地球物理研究,以分析和识别构造元素和裂缝。研究选取了Omo森林保护区、Abata Egba(沿Ondo-Ife高速公路)和Iwaraja断裂带。在垂直于断层走向的10、20和30 m电极间距处进行Wenner电极剖面,在电阻率剖面所描绘的点上采用斯伦贝谢电极配置进行垂直电测深。在奥莫森林保护区,识别出均匀高电阻率环境下的3条下降电阻率剖面断层特征。深度压裂表现为在大电极间距时电阻率值持续下降。在奥洛德地区,发现了4个签名。Iwaraja地区剖面显示净电阻率向西减小。覆盖层厚度不同,下覆基岩部分风化破碎,但不像前寒武纪结晶基底复杂环境那样具有无限电阻性。研究区是由一系列的缺点,characteriz-ed是面向北北东-南南西((NNE-SSW) directio-ns,倾向于东部。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Systematic multi-technique mapping of the Southern flank of Iwaraja fault
A geophysical study of Iwaraja segment of Ifewara-Zungeru fault zone in Nigeria was conducted using remote sensing and geoelectric techniques to analyse and identify the structural elements and fractures. The Omo Forest Reserve area, Abata Egba (along Ondo-Ife highway), and Iwaraja fault zones were selected for the study. Wenner electrode profiling was undertaken at electrode separations of 10, 20 and 30 m on diplines perpendicul-ar to trend of the fault, while Schlumberger electrode configuration was adopted for vertical electrical sounding on points delineated by resistivity profiles. At Omo Forest Reserve, 3 fault signatures of falling resistivity profi-les in uniformly high resistivity environment were identified. Deep fracturing manifested in consistently decrea-sing resistivity values at large electrode separations. At Olode area, 4 signatures were identified. The profiles at Iwaraja area showed the net resistivity decreased in Western direction. The overburden materials were variably thick and underlain by bedrock that had been partially weathered and fractured, but were not infinitely resistive as usually observed in crystalline Precambrian basement complex environment. The study area was characteriz-ed by a series of faults, which were oriented in the North North East - South South West ((NNE-SSW) directio-ns, and inclined towards the East.
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