Mineralogical and Geochemical Characterization of Arsenopyrite and Pyrite

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Geochemistry and Geochronology".

Deadline for manuscript submissions: closed (24 February 2023) | Viewed by 4096

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A. P. Vinogradov Institute of Geochemistry, Russian Academy of Sciences, 664033 Irkutsk, Russia
Interests: mineral geochemistry; physical chemistry; experiment; ore deposits; hydrothermal processes
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Guest Editor
A. P. Vinogradov Institute of Geochemistry, Russian Academy of Sciences, 664033 Irkutsk, Russia
Interests: mineral analytics; experiment; scanning probe microscopy; electron microscopy; X-ray photoelectron spectroscopy

Special Issue Information

Dear Colleagues,

Arsenopyrite (ideally FeAsS) and pyrite (FeS2) are widespread minerals in the Earth’s crust, essentially important as the scavengers of trace elements (especially gold) in ore deposits. Their abundance and commercial value has promoted the application of novel and high-efficient analytical methods to their study (SIMS, LA-ICP MS, SR XAS, APT, etc.). Nevertheless, these chemically and structurally simple compounds have remained, to date, elusive. Although there is experimental evidence that shows that pyrite and arsenopyrite are practically immiscible, the As content in natural pyrite is often very high, and the mechanism of its incorporation is not well understood. Complexity arises from the physicochemical properties of the mineral crystals due to their defect structures. The excess of metals (Fe and As) or the presence of S vacancies increases the content of noble metals, providing the formation of their “invisible” forms. The surficial nanoscale formations change geochemical characteristics, such as partition coefficients giving rise to trace element uptake. The same effect results from the intracrystalline adsorption of impurities at the boundaries of a dislocation nature.

Being excellent concentrators of gold in ore deposits, arsenopyrite and As-pyrite are fully undesirable in mine wastes because of the contamination of the environment with arsenic. On the other hand, pyrite can record bacterial processes originated at the surface of its particles, and thus holds important information on the oxygen regime of the oceans and atmosphere that took place at different stages of the Earth’s history.

For this Special Issue, we invite authors to submit original research papers as well as review articles that discuss the real structure and constitution of the minerals under consideration, which is essential not only for ore geology and mineralogy, but also for ecology, biogeochemistry and climate change science.

Dr. Vladimir Tauson
Dr. Sergey Lipko
Guest Editors

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Keywords

  • pyrite
  • arsenopyrite
  • trace element speciation
  • crystal imperfections and structural defects
  • mineral surface
  • ore deposits

Published Papers (2 papers)

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Research

16 pages, 5172 KiB  
Article
Trace Elements in Pyrite and Its Crystallization Temperature: An Example of Gold Deposits in the Darasun Goldfield, Eastern Transbaikalia, Russia
by Vsevolod Prokofiev, Valeriya Brovchenko, Lidiya Zorina, Anton Krasnov, Vera Abramova and Nikolay Bortnikov
Minerals 2023, 13(2), 288; https://doi.org/10.3390/min13020288 - 18 Feb 2023
Cited by 3 | Viewed by 2109
Abstract
The distributions of trace elements in pyrite were studied in samples of high-grade gold ores from the Talatui, Teremkyn, and Darasun deposits. The paper presents LA-ICP-MS data on concentrations of trace elements in pyrite in gold ores from mineral deposits of the Darasun [...] Read more.
The distributions of trace elements in pyrite were studied in samples of high-grade gold ores from the Talatui, Teremkyn, and Darasun deposits. The paper presents LA-ICP-MS data on concentrations of trace elements in pyrite in gold ores from mineral deposits of the Darasun goldfield, which were produced by a single fluid–magmatic system at various temperatures. The high-temperature pyrite was found to be enriched in Co, Se, and W, whereas the medium-temperature pyrite was enriched in Cu, Zn, Ag, Te, As, and In. The behaviors of some elements (Ni, Au, Bi, Sb, and Pb) seem to be independent of temperature. The identified trends and relations in the behaviors of elements can be used in studying the Au-Bi mineralization of the intrusion-related type. Full article
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14 pages, 1716 KiB  
Article
Distribution of Trace Elements (Ag, Pd, Cd, and Mn) between Pyrite and Pyrrhotite and Selectivity of Surficial Nonautonomous Phases in a Hydrothermal System
by Sergey Lipko, Vladimir Tauson, Nikolay Smagunov, Dmitriy Babkin and Irina Parkhomenko
Minerals 2022, 12(9), 1165; https://doi.org/10.3390/min12091165 - 15 Sep 2022
Cited by 2 | Viewed by 1258
Abstract
The dual distribution coefficients (D) that are related to structurally and superficially bound trace element (TE) in pyrite (Py) and pyrrhotite (Po) associations, crystallized hydrothermally at 400 °C and 1 kbar pressure, were determined. Three independent methods were used to estimate [...] Read more.
The dual distribution coefficients (D) that are related to structurally and superficially bound trace element (TE) in pyrite (Py) and pyrrhotite (Po) associations, crystallized hydrothermally at 400 °C and 1 kbar pressure, were determined. Three independent methods were used to estimate the structural and surficial TE contents (Cstr and Csur) and the corresponding D Py/Po values (Dstr and Dsur), which were found, on average, to be 12.4, 0.8, 0.9, and 0.06 (Dstr) and 2.6, 0.7, 2.0, and 0.07 (Dsur) for Ag, Pd, Cd, and Mn, respectively. The coincidence of a dual D for several elements was a result of coupled changes in Csur and Cstr. The selectivity (S) of the surficial nonautonomous phases (NAPs) that were responsible for TE accumulation (which is the ratio of TE concentrations in surficial and structural modes) was determined. It was shown that the interpretation of TE uptake by surficial phases was adequate and that this phenomenon is common in nature, independently of the system where it occurs—i.e., in experimental autoclaves or in hydrothermal ore deposits. Studies of NAPs selectivity can help in evaluating the total element compatibility in minerals and the maximum possible contents of structurally bound admixtures of the element (solubility) in minerals under given conditions. A significant surficial impurity accumulation effect is most important and well-pronounced for incompatible micro-elements with concentrations of less than ~0.1 wt%. The surficial mode may be a source of Pd and other platinum group elements and more abundant and easily refined than the structurally bound mode. Full article
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