Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set

Yuli is part of the Yankari area of the Upper Benue trough. Four important locations of warm spring are found in the area. These are namely, the Gwama Warm Spring (GWS), the Wikki Warm Spring (WWS), the Mawulgo Warm Spring (MWS) and the Tongan-Maliki Warm Spring (TWS). Identification, mapping and in...

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Main Authors: Mukaila Abdullahi, Yusufu Abubakar Sanusi, Ibrahim Nihyel Tashiwa
Format: Article
Language:English
Published: Elsevier 2025-12-01
Series:Results in Earth Sciences
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Online Access:http://www.sciencedirect.com/science/article/pii/S221171482400044X
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author Mukaila Abdullahi
Yusufu Abubakar Sanusi
Ibrahim Nihyel Tashiwa
author_facet Mukaila Abdullahi
Yusufu Abubakar Sanusi
Ibrahim Nihyel Tashiwa
author_sort Mukaila Abdullahi
collection DOAJ
description Yuli is part of the Yankari area of the Upper Benue trough. Four important locations of warm spring are found in the area. These are namely, the Gwama Warm Spring (GWS), the Wikki Warm Spring (WWS), the Mawulgo Warm Spring (MWS) and the Tongan-Maliki Warm Spring (TWS). Identification, mapping and interpretation of geological structures/features buried within the crust or exposed on the surface are important steps if not necessary in understanding the general geo-tectono-magmatism of a region. Gravity and magnetic data are employed for the interpretation of identified geologic/tectonic features/structures in the area of study. Different filtering techniques are employed. Total Horizontal Derivative of Tilt Derivative (HD_TDR), Horizontal Gradient (HG) and Generalized Derivative Operation (GDO) filters are found better option for the interpretation of the gravity data whereas for the magnetic data, First Vertical Derivative (FVD) and the Analytic Signal (AS) are found the better filters for the magnetic anomalies of the region. The study found a close connects between the normal faults in the region with the magmatic plugs and as well with the warm springs in the area. Depths to anomalous sources are recorded between 0.5 km and 4.6 km in the study area. The depth results are found from 3D Euler deconvolution inversion method.
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institution Kabale University
issn 2211-7148
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publishDate 2025-12-01
publisher Elsevier
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series Results in Earth Sciences
spelling doaj-art-382fec02703a4dc28c5e60bdd54b199f2025-01-04T04:56:19ZengElsevierResults in Earth Sciences2211-71482025-12-013100057Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-setMukaila Abdullahi0Yusufu Abubakar Sanusi1Ibrahim Nihyel Tashiwa2Physics Unit, Department of Science Laboratory Technology, Modibbo Adama University, P.M.B, Yola 2076, Nigeria; Department of Physics, Nigerian Army University, P.M.B, Biu 1500, Nigeria; Corresponding author at: Physics Unit, Department of Science Laboratory Technology, Modibbo Adama University, P.M.B, Yola 2076, Nigeria.Department of Physics, Usmanu Danfodio University, Sokoto, NigeriaDepartment of Physics, Federal University, Wukari, NigeriaYuli is part of the Yankari area of the Upper Benue trough. Four important locations of warm spring are found in the area. These are namely, the Gwama Warm Spring (GWS), the Wikki Warm Spring (WWS), the Mawulgo Warm Spring (MWS) and the Tongan-Maliki Warm Spring (TWS). Identification, mapping and interpretation of geological structures/features buried within the crust or exposed on the surface are important steps if not necessary in understanding the general geo-tectono-magmatism of a region. Gravity and magnetic data are employed for the interpretation of identified geologic/tectonic features/structures in the area of study. Different filtering techniques are employed. Total Horizontal Derivative of Tilt Derivative (HD_TDR), Horizontal Gradient (HG) and Generalized Derivative Operation (GDO) filters are found better option for the interpretation of the gravity data whereas for the magnetic data, First Vertical Derivative (FVD) and the Analytic Signal (AS) are found the better filters for the magnetic anomalies of the region. The study found a close connects between the normal faults in the region with the magmatic plugs and as well with the warm springs in the area. Depths to anomalous sources are recorded between 0.5 km and 4.6 km in the study area. The depth results are found from 3D Euler deconvolution inversion method.http://www.sciencedirect.com/science/article/pii/S221171482400044XAeromagnetic dataGlobal gravity dataGeological structures/featuresWarm springsVolcanic plugsEdge detection filters
spellingShingle Mukaila Abdullahi
Yusufu Abubakar Sanusi
Ibrahim Nihyel Tashiwa
Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set
Results in Earth Sciences
Aeromagnetic data
Global gravity data
Geological structures/features
Warm springs
Volcanic plugs
Edge detection filters
title Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set
title_full Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set
title_fullStr Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set
title_full_unstemmed Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set
title_short Structural investigations of Yuli Geothermal field in Nigeria using gravity and magnetic data-set
title_sort structural investigations of yuli geothermal field in nigeria using gravity and magnetic data set
topic Aeromagnetic data
Global gravity data
Geological structures/features
Warm springs
Volcanic plugs
Edge detection filters
url http://www.sciencedirect.com/science/article/pii/S221171482400044X
work_keys_str_mv AT mukailaabdullahi structuralinvestigationsofyuligeothermalfieldinnigeriausinggravityandmagneticdataset
AT yusufuabubakarsanusi structuralinvestigationsofyuligeothermalfieldinnigeriausinggravityandmagneticdataset
AT ibrahimnihyeltashiwa structuralinvestigationsofyuligeothermalfieldinnigeriausinggravityandmagneticdataset