尼日利亚东南部埃努古州Isu-Awaa裂缝带二维电阻率成像

C. Chukwudi, O. Nneka, C. O. Austin
{"title":"尼日利亚东南部埃努古州Isu-Awaa裂缝带二维电阻率成像","authors":"C. Chukwudi, O. Nneka, C. O. Austin","doi":"10.5897/ijps2022.4985","DOIUrl":null,"url":null,"abstract":"2D electrical resistivity imaging technique has been used to investigate the nature and dimensions of the fracture prone zones in Isu-Awaa, Enugu State, Nigeria. The study area lies within Latitude 06° 14 I 0 II N to 06° 17 I 0 II N and Longitudes 007° 23 I 0 II E to 007° 28 I 0 II E, with an area extent of about 51 Km 2 . The area is underlain by three main geological units (Enugu Shale, Owelli Sandstone and Mamu Formation). The study area is topographically undulating with high ridges surrounding the area. 2D electrical resistivity data was acquired with Wenner configuration, employing the roll-along technique to image the subsurface. A total of four (4) number 2D electrical resistivity imaging traverses were carried out. Data was processed and interpreted using RES2DINV. Measured and calculated apparent resistivity pseudo sections were convolved to generate the inverse model resistivity section, which was the diagnostic interpretative model used. Discontinuities in the layering are possible fracture zones. Major discontinuities were observed at distances of 48 and 87, 52.5, 106, 8.0 and 26 m at traverses A, B, C and D respectively. Fracture trend azimuth rose diagram, shows pre-dominant trend to the SE direction with minority to the SW and NW, and relicts to the NE directions. This conforms to the regional lineaments map of Nigeria. The use of 2D electrical resistivity imaging tool has proved useful in the mapping of fracture prone zones in the study area.","PeriodicalId":14294,"journal":{"name":"International Journal of Physical Sciences","volume":"9 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-08-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"2D electrical resistivity imaging of fracture zones in Isu-Awaa, Enugu State, Southeastern Nigeria\",\"authors\":\"C. Chukwudi, O. Nneka, C. O. Austin\",\"doi\":\"10.5897/ijps2022.4985\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"2D electrical resistivity imaging technique has been used to investigate the nature and dimensions of the fracture prone zones in Isu-Awaa, Enugu State, Nigeria. The study area lies within Latitude 06° 14 I 0 II N to 06° 17 I 0 II N and Longitudes 007° 23 I 0 II E to 007° 28 I 0 II E, with an area extent of about 51 Km 2 . The area is underlain by three main geological units (Enugu Shale, Owelli Sandstone and Mamu Formation). The study area is topographically undulating with high ridges surrounding the area. 2D electrical resistivity data was acquired with Wenner configuration, employing the roll-along technique to image the subsurface. A total of four (4) number 2D electrical resistivity imaging traverses were carried out. Data was processed and interpreted using RES2DINV. Measured and calculated apparent resistivity pseudo sections were convolved to generate the inverse model resistivity section, which was the diagnostic interpretative model used. Discontinuities in the layering are possible fracture zones. Major discontinuities were observed at distances of 48 and 87, 52.5, 106, 8.0 and 26 m at traverses A, B, C and D respectively. Fracture trend azimuth rose diagram, shows pre-dominant trend to the SE direction with minority to the SW and NW, and relicts to the NE directions. This conforms to the regional lineaments map of Nigeria. The use of 2D electrical resistivity imaging tool has proved useful in the mapping of fracture prone zones in the study area.\",\"PeriodicalId\":14294,\"journal\":{\"name\":\"International Journal of Physical Sciences\",\"volume\":\"9 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-08-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"International Journal of Physical Sciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5897/ijps2022.4985\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Journal of Physical Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5897/ijps2022.4985","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

摘要

2D电阻率成像技术已被用于调查尼日利亚埃努古州Isu-Awaa裂缝易发带的性质和规模。研究区位于北纬06°14°0°N ~ 06°17°0°N和东经007°23°0°E ~ 007°28°0°E范围内,面积约51 km2。该地区由三个主要地质单元(Enugu页岩、Owelli砂岩和Mamu组)组成。研究区地形起伏,周围有高高的山脊。采用Wenner配置获取二维电阻率数据,采用沿滚技术对地下进行成像。共进行了4次二维电阻率成像遍历。使用RES2DINV对数据进行处理和解释。将实测和计算的视电阻率伪剖面进行卷积得到电阻率反演模型剖面,作为诊断解释模型。层理中的不连续面是可能的断裂带。在A、B、C和D处,分别在48和87、52.5、106、8.0和26 m处观测到主要不连续性。裂缝走向方位角上升图显示,裂缝走向以东南方向为主,西南、西北方向占少数,其余为东北方向。这符合尼日利亚的区域线形图。事实证明,二维电阻率成像工具在研究区域的裂缝易发带测绘中非常有用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
2D electrical resistivity imaging of fracture zones in Isu-Awaa, Enugu State, Southeastern Nigeria
2D electrical resistivity imaging technique has been used to investigate the nature and dimensions of the fracture prone zones in Isu-Awaa, Enugu State, Nigeria. The study area lies within Latitude 06° 14 I 0 II N to 06° 17 I 0 II N and Longitudes 007° 23 I 0 II E to 007° 28 I 0 II E, with an area extent of about 51 Km 2 . The area is underlain by three main geological units (Enugu Shale, Owelli Sandstone and Mamu Formation). The study area is topographically undulating with high ridges surrounding the area. 2D electrical resistivity data was acquired with Wenner configuration, employing the roll-along technique to image the subsurface. A total of four (4) number 2D electrical resistivity imaging traverses were carried out. Data was processed and interpreted using RES2DINV. Measured and calculated apparent resistivity pseudo sections were convolved to generate the inverse model resistivity section, which was the diagnostic interpretative model used. Discontinuities in the layering are possible fracture zones. Major discontinuities were observed at distances of 48 and 87, 52.5, 106, 8.0 and 26 m at traverses A, B, C and D respectively. Fracture trend azimuth rose diagram, shows pre-dominant trend to the SE direction with minority to the SW and NW, and relicts to the NE directions. This conforms to the regional lineaments map of Nigeria. The use of 2D electrical resistivity imaging tool has proved useful in the mapping of fracture prone zones in the study area.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
International Journal of Physical Sciences
International Journal of Physical Sciences 综合性期刊-综合性期刊
自引率
0.00%
发文量
4
审稿时长
24 months
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信