Determination of Source of Gold around Itagunmodi Southwest, Nigeria

The source of gold mineralization had been a subject of proposal in the past; some researchers suggested its original source to be the crust while some proposed the source as the mantle. In this study, the source of gold in Itagunmodi was the main objective. The melting temperature of gold and the variation of melting temperature with increase in pressures were determined from melting temperature equations and the values were correlated with the stress in the lithosphere to determine the source. At high values of pressures, the gold melts at higher temperatures. The melting temperatures ranged between 1064 ℃ to 1394.3 ℃ while pressure ranged between 2605.68-2931.39 MPα, (i.e 26-29 Kbar). When merged with the temperature and stress field in the Earth, its shows that the source of gold mineralization around the location is the mantle part of the lithosphere and this can serve as the baseline to the source of gold which was believed to originate from the mantle.

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Publication Details

Journal
Asian Journal of Science Technology Engineering and Art
Published
2025-03-01
DOI
https://doi.org/10.58578/ajstea.v3i2.5063
Primary Topic
Geochemistry and Geologic Mapping
Type
article
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article

Determination of Source of Gold around Itagunmodi Southwest, Nigeria

Aminu K. Bello, A. A. Adetoyinbo
Asian Journal of Science Technology Engineering and Art
Geochemistry and Geologic Mapping
article

Determination of Source of Gold around Itagunmodi Southwest, Nigeria

Aminu K. Bello, A. A. Adetoyinbo
article en

Abstract

The source of gold mineralization had been a subject of proposal in the past; some researchers suggested its original source to be the crust while some proposed the source as the mantle. In this study, the source of gold in Itagunmodi was the main objective. The melting temperature of gold and the variation of melting temperature with increase in pressures were determined from melting temperature equations and the values were correlated with the stress in the lithosphere to determine the source. At high values of pressures, the gold melts at higher temperatures. The melting temperatures ranged between 1064 ℃ to 1394.3 ℃ while pressure ranged between 2605.68-2931.39 MPα, (i.e 26-29 Kbar). When merged with the temperature and stress field in the Earth, its shows that the source of gold mineralization around the location is the mantle part of the lithosphere and this can serve as the baseline to the source of gold which was believed to originate from the mantle.

Asian Journal of Science Technology Engineering and ArtVol. 3(2)
Bells University of Technology (NG), University of Ibadan (NG)
Openalex Percentile: Top 99%
Geochemistry and Geologic Mapping
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