Investigating the applicability of the social spider optimization for the inversion of magnetic anomalies caused by dykes

Ben, Ubong C.; Mbonu, Charles Chisom; Thompson, Cherish Edet; Ekwok, Stephen E.; Akpan, Anthony E.; Akpabio, Idara; Eldosouky, Ahmed M.; Abdelrahman, Kamal; Al-Zahrani, Hassan S.; Gómez-Ortíz, David; Pham, Luan Thanh

doi:10.1016/j.jksus.2023.102569

Cited by 4 publications

(5 citation statements)

References 21 publications

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“… Interpret dykes from magnetic anomaly is difficult without applying advanced algorithm methods like Social Spider Optimization (SSO). joint inversions depending on the physical property's empirical relationship parameters include certain limitations [ 16 , 17 , 25 , 35 , [78] , [79] , [80] ]. …”

Section: Methodsmentioning

confidence: 99%

“…joint inversions depending on the physical property's empirical relationship parameters include certain limitations [ 16 , 17 , 25 , 35 , [78] , [79] , [80] ].…”

Section: Methodsmentioning

confidence: 99%

“… Synthetic and field data could utilized to validate the effectiveness and correctness of the developed nonlinear inverse algorithms. The ability of high resolution and rapid inversions is a crucial prerequisite for the inversion's practical application without either limiting or data down-sampling the resolution or size of the inversion domain [ 16 , 17 , 24 , 25 , 67 , 69 , 72 , 78 , 108 ]. …”

Section: Methodsmentioning

confidence: 99%

“…The ability of high resolution and rapid inversions is a crucial prerequisite for the inversion's practical application without either limiting or data down-sampling the resolution or size of the inversion domain [ 16 , 17 , 24 , 25 , 67 , 69 , 72 , 78 , 108 ].…”

Section: Methodsmentioning

confidence: 99%

“…Zhang et al [ 77 ] applied three-component magnetic anomalies, introduced an Occam-type inversion algorithm into a spherical coordinate system, and inverted the magnetization. Eventually, for the inversion of magnetic anomalies caused by dykes, a social spider optimization (SPO) algorithm was developed to decipher the source body properties tested with synthetic anomalies corrupted by different levels of random noise and field anomalies [ 35 , [78] , [79] , [80] ]. Finally, as new research, a 3D inverse modeling procedure was applied to the Charmaleh Iron deposit magnetic data in Iran to obtain a valid anomaly edge perimeter.…”

Section: Introductionmentioning

confidence: 99%

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Geobody estimation by Bhattacharyya method utilizing nonlinear inverse modeling of magnetic data in Baba-Ali iron deposit, NW Iran

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et al. 2023

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Section: Methodsmentioning

confidence: 99%

“…joint inversions depending on the physical property's empirical relationship parameters include certain limitations [ 16 , 17 , 25 , 35 , [78] , [79] , [80] ].…”

Section: Methodsmentioning

confidence: 99%

Section: Methodsmentioning

confidence: 99%

Section: Methodsmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Geobody estimation by Bhattacharyya method utilizing nonlinear inverse modeling of magnetic data in Baba-Ali iron deposit, NW Iran

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Unveiling the mineral resources and structural patterns in the Middle Benue Trough: a comprehensive exploration using airborne magnetic and radiometric data

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Exploratory Mapping of the Geothermal Anomalies in the Neoproterozoic Arabian Shield, Saudi Arabia, Using Magnetic Data

et al. 2023

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In this paper, certain areas of the Kingdom of Saudi Arabia (KSA) are assessed in order to map potential geothermal energy zones. To evaluate high-resolution aerial magnetic data, spectral depth analysis using a modified centroid approach was used. The calculated geothermal parameters were gridded in order to delineate the regions characterised by a shallow Curie point depth (CPD) and a high geothermal gradient (GG) as well as a high heat flow (HF). The CPD, GG and HF calculated from the analysed data varied in the ranges of 6.0–15.0 km, 40.0–100.0 °C/km and 90.0–270.0 mW/m2, respectively. The obtained results show the concurrence of the positions of shallow CPD (<8.0 km), high GG (>83.5 °C/km) and high HF (>211.0 mW/m2). The geothermal systems that are oriented in the E–W direction are related to the Red Sea tectonics, the tectonic opening of the Red Sea/Gulf of the Suez Rift, hot subterranean anomalies and high enthalpy from radioactive granites. Likewise, the geologic structures (fractures and faults) related to the Red Sea tectonics serve as channels for the movement of hydrothermal fluids and the deposition of associated minerals. All in all, another geophysical study involving deep boreholes, and seismic, magnetotelluric, electromagnetic and geochemical data should be conducted to evaluate and estimate precisely the economic reserves of geothermal resources.

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Investigating the applicability of the social spider optimization for the inversion of magnetic anomalies caused by dykes

Cited by 4 publications

References 21 publications

Geobody estimation by Bhattacharyya method utilizing nonlinear inverse modeling of magnetic data in Baba-Ali iron deposit, NW Iran

Geobody estimation by Bhattacharyya method utilizing nonlinear inverse modeling of magnetic data in Baba-Ali iron deposit, NW Iran

Unveiling the mineral resources and structural patterns in the Middle Benue Trough: a comprehensive exploration using airborne magnetic and radiometric data

Exploratory Mapping of the Geothermal Anomalies in the Neoproterozoic Arabian Shield, Saudi Arabia, Using Magnetic Data

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