Characterization of talc deposits in ultramafic rocks of Gebel El Maiyit and its economic feasibility

A comprehensive, multiscale investigation, integrating remote sensing, mineralogy, whole rock chemistry, Electron Microprobe (EMP), and stable isotopes (oxygen-<sup>18</sup>O and carbon-<sup>13</sup>C), was undertaken to assess the feasibility of talc deposits and their host serpentinite at Gebel El-Maiyit in the Eastern Desert of Egypt. Sentinel 2 remote sensing images were applied to discriminate talc from serpentinites followed by geochemical study of serpentinites using RO`/SiO<sub>2</sub> ratios, AFM diagram and MgO versus SiO<sub>2</sub> relationship indicates a peridotite origin formed at low temperature Alpine type. Our study revealed that talc deposit has a varied mineralogical composition and according to the predominant talc and gangue minerals three main types have been distinguished: 1- pure talc, 2- tremolite talc and 3- chlorite talc. Paragenetically, talc is derived from serpentine minerals, tremolite and chlorite. The latter is formed at about 231 °C. The chemical data of talc deposit reveals that the summation of talc components (SiO<sub>2</sub> + MgO + H<sub>2</sub>O) is 92.68%, while that of impurity oxides (Al<sub>2</sub>O<sub>3</sub> + CaO + Fe<sub>2</sub>O<sub>3</sub> + FeO) is 5.56%. The carbon<sup>13</sup>C) and oxygen<sup>18</sup>O) contents of pure magnesite revealed that the pure phase of Gebel El-Maiyit was formed at low temperature (around 100 °C) while magnesite contained in talc carbonate rock was formed at high temperature (140-175 °C). In terms of source fluids, the metamorphic and /or magmatic water was supposed to be the main fluids which are circulated during the hydrothermal alteration. Although S and P are very minor components in all the talc ore types of the considered area and do not affect their industrial use. Copper (Cu) was not detected. Iron (Fe) and manganese (Mn) concentrations are significantly high, necessitating treatment to reduce these elements for the ore to be suitable as an electrical insulator. Arsenic (As) levels are consistently below 5 ppm, indicating the ore's potential use in the cosmetic industry without further processing.

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Journal
Scientific Reports
Published
2025-04-24
DOI
https://doi.org/10.1038/s41598-025-97465-7
Primary Topic
Geochemistry and Geologic Mapping
Type
article
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article

Characterization of talc deposits in ultramafic rocks of Gebel El Maiyit and its economic feasibility

Samir M. Aly, Ibrahim A. Salem, Ali Shebl, Ismail A. Thabet
Scientific Reports
Geochemistry and Geologic Mapping
article

Characterization of talc deposits in ultramafic rocks of Gebel El Maiyit and its economic feasibility

Samir M. Aly, Ibrahim A. Salem, Ali Shebl, Ismail A. Thabet
article en

Abstract

A comprehensive, multiscale investigation, integrating remote sensing, mineralogy, whole rock chemistry, Electron Microprobe (EMP), and stable isotopes (oxygen-<sup>18</sup>O and carbon-<sup>13</sup>C), was undertaken to assess the feasibility of talc deposits and their host serpentinite at Gebel El-Maiyit in the Eastern Desert of Egypt. Sentinel 2 remote sensing images were applied to discriminate talc from serpentinites followed by geochemical study of serpentinites using RO`/SiO<sub>2</sub> ratios, AFM diagram and MgO versus SiO<sub>2</sub> relationship indicates a peridotite origin formed at low temperature Alpine type. Our study revealed that talc deposit has a varied mineralogical composition and according to the predominant talc and gangue minerals three main types have been distinguished: 1- pure talc, 2- tremolite talc and 3- chlorite talc. Paragenetically, talc is derived from serpentine minerals, tremolite and chlorite. The latter is formed at about 231 °C. The chemical data of talc deposit reveals that the summation of talc components (SiO<sub>2</sub> + MgO + H<sub>2</sub>O) is 92.68%, while that of impurity oxides (Al<sub>2</sub>O<sub>3</sub> + CaO + Fe<sub>2</sub>O<sub>3</sub> + FeO) is 5.56%. The carbon<sup>13</sup>C) and oxygen<sup>18</sup>O) contents of pure magnesite revealed that the pure phase of Gebel El-Maiyit was formed at low temperature (around 100 °C) while magnesite contained in talc carbonate rock was formed at high temperature (140-175 °C). In terms of source fluids, the metamorphic and /or magmatic water was supposed to be the main fluids which are circulated during the hydrothermal alteration. Although S and P are very minor components in all the talc ore types of the considered area and do not affect their industrial use. Copper (Cu) was not detected. Iron (Fe) and manganese (Mn) concentrations are significantly high, necessitating treatment to reduce these elements for the ore to be suitable as an electrical insulator. Arsenic (As) levels are consistently below 5 ppm, indicating the ore's potential use in the cosmetic industry without further processing.

Scientific ReportsVol. 15(1)
Tanta University (EG)
Debreceni Egyetem, Nemzeti Kutatási Fejlesztési és Innovációs Hivatal, U.S. Geological Survey
Peace, Justice and strong institutions
Openalex Percentile: Top 96%
Geochemistry and Geologic Mapping
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