Evidence map›Paper›PMID 42014875›Full record

ArticleScientific reports2026

Geophysical characterization of subsurface structures for optimal planning in the Abu Tartur phosphate mine.

Gehad M K Ahmed, M M Senosy, Gamal Y Boghdady, Mosaad Ali Hussein Ali

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Article in Scientific reports, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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1 · What the graph read from it

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2 · The registry

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4 · The record

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5 · Who and what money

Authors and funding

4 authors.

Gehad M K AhmedDepartment of Mining and Metallurgical Engineering, Faculty of Engineering, Assiut University, Assiut, Egypt. gehad.mostafa@aun.edu.eg.
M M SenosyGeology Department, Faculty of Science, Assiut University, Assiut, Egypt.
Gamal Y BoghdadyDepartment of Mining and Metallurgical Engineering, Faculty of Engineering, Assiut University, Assiut, Egypt.
Mosaad Ali Hussein AliDepartment of Mining and Metallurgical Engineering, Faculty of Engineering, Assiut University, Assiut, Egypt. mossad_ali2000@aun.edu.eg.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Optimal planning of the Abu Tartur Mine (ATPM) in Egypt requires a comprehensive understanding of the region’s phosphate ore geology. The recent closure of the subsurface ATPM was primarily due to insufficient geological data, including unrecognized faults that concealed phosphate beds. The present study integrates gravity and magnetic geophysical methods to characterize the phosphate beds and identify geological structures. Aeromagnetic Reduced to Pole (RTP) and Bouguer anomaly data were used, with filters (analytical signal, first vertical derivative, high-pass and low-pass (applied to enhance interpretation. Through 2D gravity and magnetic modelling, the subsurface sedimentary sequence above the basement rocks was defined. The subsea depth to the subsurface rock layer boundaries was determined. Consequently, structure contour maps were created for the basement and the Nubian sandstone surfaces, along with Isopach map of the phosphatic rocks. Maps and filtered data revealed the predominant subsurface structures controlling the phosphate distribution. These structures are folds (plunging and double-plunging synclines and anticlines with axes trending NE-SW, NNW-SSE, and NW-SE) and faults (normal and strike-slip). Normal faults bound the ATPM plateau with downthrow directions outward. The thickness of phosphatic rocks varies from 0.8 to 32 m. The limited thickness is recorded in the present ATPM location, whereas the maximum thickness is observed at the troughs of the syncline folds located northeast and southwest of the plateau. Therefore, the ATPM location was suboptimal and uneconomical, while the northeast and southwest areas offer more promising targets for phosphate extraction. This misallocation likely contributed to the mine failure.

Indexed as

Abu Tartur mineAeromagneticBouguer gravitySubsurface structures

Identifiers

PMID42014875
PMCPMC13099985

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