Role of impurities in the semiconducting properties of natural pyrite: Implications for the electrochemical accumulation of visible gold and formation of hydrothermal gold deposits
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Baisong Du
, M. Santosh
Abstract
Pyrite (FeS2), the most abundant sulfide mineral on Earth, typically contains a host of minor and trace elements, including As, Co, Ni, and Au. It is an important semiconductor with unique structural properties markedly influenced by elemental impurities. However, whether the change in semiconducting properties of natural pyrite is caused by the type and concentration of trace elements or by a non-stoichiometry-related doping mechanism remains uncertain. Moreover, the effect of semiconducting properties on the enrichment mechanism of Au has not been well addressed. Here, we investigate microscopic pyrite crystals from the Heilangou gold field (HGF) in the eastern Jiaodong Peninsula using field emission scanning electron microscopy (SEM), electron probe microanalysis (EPMA), in situ laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS), potential-Seebeck microprobe (PSM), and thermoelectric measurements. The results demonstrate that pyrite grains show either p- or n-type conductivity depending on chemical compositions. Pyrite enriched in As, which typically substitutes for S in the crystal structure, tends to be p-type with a positive Seebeck coefficient, whereas pyrite crystals enriched in Co, Ni, Cu, and Zn, as well as those depleted in As, are typically n-type. Moreover, As shows the strongest influence on the semiconducting properties of natural pyrite crystals and a strong positive correlation with Au. We observed that visible Au grains are preferentially accumulated on individual domains of sulfides (e.g., As-rich pyrite) that act as cathodes, suggesting that electrical p-n junctions in sulfides drive electrochemical reactions with ore-forming fluids, resulting in the deposition of visible Au. The electrochemical precipitation mechanism of Aumay account for the formation of other types of hydrothermal Au deposits.
Acknowledgments and Funding
We gratefully thank R. Large, associate editor Daniel Gregory, and two anonymous reviewers for their critical and constructive comments, which significantly improved the manuscript. Fangyue Wang (Hefei University of Technology) and Qian Mao (Chinese Academy of Sciences) are thanked for their technical assistance with the LA-ICP-MS and EPMA analyses. This research was financially supported by the National Nature Science Foundation of China (No. 42130801) and the Science Basic Research Program of Shananxi (No. 2014JC-YBQN-0350).
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Articles in the same Issue
- Gender in mineral names
- Role of impurities in the semiconducting properties of natural pyrite: Implications for the electrochemical accumulation of visible gold and formation of hydrothermal gold deposits
- Unraveling clay-mineral genesis and climate change on Earth and Mars using machine learning-based VNIR spectral modeling
- Characteristics of the distribution of minerals among the space groups
- Al3+ and H+ substitutions in TiO2 polymorphs: Structural and vibrational investigations
- Oriented triphylite rods in apatite from an LCT pegmatite in the Stankuvatske Li-ore deposit, Ukraine: Implications for Li mobility
- Quartz textures, trace elements, fluid inclusions, and in situ oxygen isotopes from Aktogai porphyry Cu deposit, Kazakhstan
- Cu nanoparticle geometry as the key to bicolor behavior in Oregon sunstones: An application of LSPR theory in nanomineralogy
- Gowerite, Ca[B5O8(OH)][B(OH)3]·3H2O: Revisiting the crystal structure and exploring its formation context
- Zhonghongite, Cu29(As, Sb)12S33, a new mineral from the high-sulfidation vein of Jiama porphyry system, Tibet, China
- Uramphite, (NH4)(UO2)(PO4)·3H2O, from the second world occurrence, Beshtau uranium deposit, Northern Caucasus, Russia: Crystal-structure refinement, infrared spectroscopy, and relation to uramarsite
- A simple method to create mineral mounts in thin section for teaching optical mineralogy
Articles in the same Issue
- Gender in mineral names
- Role of impurities in the semiconducting properties of natural pyrite: Implications for the electrochemical accumulation of visible gold and formation of hydrothermal gold deposits
- Unraveling clay-mineral genesis and climate change on Earth and Mars using machine learning-based VNIR spectral modeling
- Characteristics of the distribution of minerals among the space groups
- Al3+ and H+ substitutions in TiO2 polymorphs: Structural and vibrational investigations
- Oriented triphylite rods in apatite from an LCT pegmatite in the Stankuvatske Li-ore deposit, Ukraine: Implications for Li mobility
- Quartz textures, trace elements, fluid inclusions, and in situ oxygen isotopes from Aktogai porphyry Cu deposit, Kazakhstan
- Cu nanoparticle geometry as the key to bicolor behavior in Oregon sunstones: An application of LSPR theory in nanomineralogy
- Gowerite, Ca[B5O8(OH)][B(OH)3]·3H2O: Revisiting the crystal structure and exploring its formation context
- Zhonghongite, Cu29(As, Sb)12S33, a new mineral from the high-sulfidation vein of Jiama porphyry system, Tibet, China
- Uramphite, (NH4)(UO2)(PO4)·3H2O, from the second world occurrence, Beshtau uranium deposit, Northern Caucasus, Russia: Crystal-structure refinement, infrared spectroscopy, and relation to uramarsite
- A simple method to create mineral mounts in thin section for teaching optical mineralogy