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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (1/1 displayed)

  • 2024Chemical Reactivity and Alteration of Pyrite Mineral in the Kubi Gold Concession in Ghana1citations

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Magnuson, Martin
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Hultman, Lars
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Yaya, Abu
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Nzulu, Gabriel Kofi
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Högberg, Hans
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Eklund, Per
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2024

Co-Authors (by relevance)

  • Magnuson, Martin
  • Hultman, Lars
  • Yaya, Abu
  • Nzulu, Gabriel Kofi
  • Högberg, Hans
  • Eklund, Per
OrganizationsLocationPeople

article

Chemical Reactivity and Alteration of Pyrite Mineral in the Kubi Gold Concession in Ghana

  • Magnuson, Martin
  • Hultman, Lars
  • Nude, Prosper M.
  • Yaya, Abu
  • Nzulu, Gabriel Kofi
  • Högberg, Hans
  • Eklund, Per
Abstract

<jats:title>Abstract</jats:title><jats:p>Pyrite is the most common among the group of sulfide minerals in the Earth and abundant in most geological settings. This gangue mineral in association with garnet, hematite, magnetite, and other sulfide minerals acts as an indicator mineral in the Kubi concession of the Asante Gold corporation in Ghana. X-ray diffraction (XRD), air annealing in a furnace, energy-dispersive x-ray spectroscopy (EDX), and X-ray photoelectron spectroscopy (XPS) were applied to investigate the crystal structure, identify individual elements, permanence, transformation, and chemical/electronic properties of such pyrite. The study aims to identify individual elements and to gain an understanding of the surface reaction mechanisms, as well as the properties of precipitated pyrite particles observed during the hydrothermal formation of the ore deposit. XRD shows that pristine and annealed samples contain some hematite and quartz besides pyrite. Results from air annealing indicate that the relationship between pyrite and hematite-magnetite is controlled by temperature. EDX reveals that the sample has O and C as contaminants, while XPS in addition reveals Ba, Au, P, Al, and N. These elements are attributed to pyrite that bonds metallically or covalently to neighboring ligands/impurity minerals such as oxides, chalcogenide sulfides, as well as the gangue alteration minerals of magnetite and hematite in the pyrite sample.</jats:p><jats:p>These findings suggest that during the hydrothermal flow regime, pyrite, pathfinder elements, and impurity minerals/metals were in contact with quartz minerals before undergoing hematite transformation, which thus becomes an indicator mineral in the Kubi gold concession.</jats:p>

Topics
  • impedance spectroscopy
  • mineral
  • surface
  • x-ray diffraction
  • x-ray photoelectron spectroscopy
  • gold
  • annealing
  • Energy-dispersive X-ray spectroscopy