Radiometric characteristics of some metallic ores and nonmetallic deposits: an example, Wadi Al-Allaqi, South Eastern Desert, Egypt

Mohamed Mostafa Gobashy; Mohamed A El-Sadek; Mahmoud M Mekkawi; Sultan Awad Sultan Araffa; Mohamed M Ezz Eldin; Mohamed Hassan Khalil

doi:10.1038/s41598-024-52912-9

Radiometric characteristics of some metallic ores and nonmetallic deposits: an example, Wadi Al-Allaqi, South Eastern Desert, Egypt

Sci Rep. 2024 Jan 30;14(1):2443. doi: 10.1038/s41598-024-52912-9.

Authors

Mohamed Mostafa Gobashy¹, Mohamed A El-Sadek², Mahmoud M Mekkawi³, Sultan Awad Sultan Araffa³, Mohamed M Ezz Eldin⁴, Mohamed Hassan Khalil⁵

Affiliations

¹ Geophysics Department, Faculty of Science, Cairo University, Giza, Egypt. Gobashy@sci.cu.edu.eg.
² Nuclear Materials Authority, Maadi-Kattamia Road, P.O. Box 530, Cairo, Egypt.
³ National Research Institute of Astronomy and Geophysics (NRIAG), Helwan, Cairo, Egypt.
⁴ Egyptian Mineral Recourses Authority (EMRA), Cairo, Egypt.
⁵ Geophysics Department, Faculty of Science, Cairo University, Giza, Egypt.

Abstract

Hydrothermal alteration processes are connected to many mineral formations, particularly auriferous deposits. In this study, airborne gamma-ray spectrometry (GRS) data and the analysis of radioactive materials (eU, eTh, and K) are applied to search for regions with hydrothermal alteration activity. An example is presented from Wadi Al-Allaqi, South Eastern Desert, Egypt. GRS was used to analyse various radiometric data to address potential mineral deposit areas, to map regions potentially showing metallic ore mineralisation, and to point out new geological mineral resources. The Kd (potassium deviation), "F" parameter and Th-normalisation of the K and eU anomalies were calculated, and locating new exploratory targets in the study area that exhibit high F-parameter, Kd, and K/eTh values was recommended. Additionally, the research region has a few isolated enriched spots of (K). Therefore, GRS data was used to characterise and estimate potential metallic ores, nonmetallic deposits, and gold ore zones associated with the alteration zones. Results show that most of the known mineral deposits and gold occurrences in the area, according to the metallogenic map of Egypt, are located in zones with a ratio value of (0.25-0.30) (K%/(U or Th ppm)) maps which may suggest a moderate degree of alteration. Also, most mineral deposits and gold occurrences are found in intermediate altered zones, or K-enriched sites, with a Kd% of (0.2. The work represents an attempt to map hydrothermal alteration zones associated with mineral deposits in the Wadi Al-Allaqi area. Generally, natural radiation characteristics and attributes suggest criteria that can be used globally for regional mineral exploration.