Toward the continuous series of HgS-ZnS solid solutions: Zn-rich metacinnabar assemblages in the Vorontsovskoe gold deposit, Northern Urals, Russia

Abstract A nearly continuous series of metacinnabar–sphalerite solid solutions is reported in assemblages of Zn-rich metacinnabar in gold-bearing carbonate breccias of the Vorontsovskoe gold deposit, Northern Urals, Russia. Metacinnabar occurs as grains containing paragenetic inclusions of realgar, specific thallium-bearing sulfosalts, high-fineness native gold, and various ZnS–HgS minerals, including Zn-bearing metacinnabar, Hg-bearing sphalerite, and pure cinnabar. Selected metacinnabar-sphalerite compositions fall within the (Hg0.54Zn0.46)S–(Zn0.62Hg0.38)S range. This finding confirms the absence of the long-debated miscibility gap (MG), which was previously constrained to (Hg0.54Zn0.46)S–(Zn0.75Hg0.25)S in the natural HgS–ZnS cubic system. The compositions obtained within the MG have the following major components ranges (wt%): Zn (17.7–27.3), Hg (50.7–63.6), and S (18.7–22.0). Compositional zoning in Zn and Hg contents is observed in metacinnabar. The core consists of either highly Hg-enriched sphalerite or Zn-enriched metacinnabar, while the rim is composed of low-Zn metacinnabar (3–5 wt% Zn). The Hg/Zn ratio gradually increases from core to periphery. Metacinnabar also contains minor impurities of Mn (up to 1.2 wt%) and Cd (up to 2.6 wt%). Mn is a nearly constant constituent. Based on published compositional data on sphalerite-metacinnabar from 38 localities, Mn is considered an indicator for these minerals in Vorontsovskoe. Zoned Zn- and Mn-bearing metacinnabar formed during cooling (from <350 °C to <200 °C) of late-stage hydrothermal fluids enriched in chalcophile Tl-Cu-Zn-Hg-As-Sb-S elements. Our study suggests that a complete series of ZnS–HgS solid solutions may be found in hydrothermal systems with a relatively high-temperature formation regime (>250 °C). In addition, Zn-Mn-bearing metacinnabar is a metastable phase in the Zn-Hg-Mn-S system. Mn is considered a stabilizer for metacinnabar, a natural counterpart of β-HgS, which is a prospective zero-gap semiconductor.

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Journal
American Mineralogist
Published
2025-09-18
DOI
https://doi.org/10.2138/am-2025-9783
Primary Topic
Geological and Geochemical Analysis
Type
article
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article

Toward the continuous series of HgS-ZnS solid solutions: Zn-rich metacinnabar assemblages in the Vorontsovskoe gold deposit, Northern Urals, Russia

M.A. Rassomakhin, Dmitry A. Artemyev, Sergey N. Britvin, V. S. et al.
American Mineralogist
Geological and Geochemical Analysis
article

Toward the continuous series of HgS-ZnS solid solutions: Zn-rich metacinnabar assemblages in the Vorontsovskoe gold deposit, Northern Urals, Russia

M.A. Rassomakhin, Dmitry A. Artemyev, Sergey N. Britvin, V. S., F. D. Sandalov, Е. В. Белогуб, S. Yu. Stepanov
article en

Abstract

Abstract A nearly continuous series of metacinnabar–sphalerite solid solutions is reported in assemblages of Zn-rich metacinnabar in gold-bearing carbonate breccias of the Vorontsovskoe gold deposit, Northern Urals, Russia. Metacinnabar occurs as grains containing paragenetic inclusions of realgar, specific thallium-bearing sulfosalts, high-fineness native gold, and various ZnS–HgS minerals, including Zn-bearing metacinnabar, Hg-bearing sphalerite, and pure cinnabar. Selected metacinnabar-sphalerite compositions fall within the (Hg0.54Zn0.46)S–(Zn0.62Hg0.38)S range. This finding confirms the absence of the long-debated miscibility gap (MG), which was previously constrained to (Hg0.54Zn0.46)S–(Zn0.75Hg0.25)S in the natural HgS–ZnS cubic system. The compositions obtained within the MG have the following major components ranges (wt%): Zn (17.7–27.3), Hg (50.7–63.6), and S (18.7–22.0). Compositional zoning in Zn and Hg contents is observed in metacinnabar. The core consists of either highly Hg-enriched sphalerite or Zn-enriched metacinnabar, while the rim is composed of low-Zn metacinnabar (3–5 wt% Zn). The Hg/Zn ratio gradually increases from core to periphery. Metacinnabar also contains minor impurities of Mn (up to 1.2 wt%) and Cd (up to 2.6 wt%). Mn is a nearly constant constituent. Based on published compositional data on sphalerite-metacinnabar from 38 localities, Mn is considered an indicator for these minerals in Vorontsovskoe. Zoned Zn- and Mn-bearing metacinnabar formed during cooling (from <350 °C to <200 °C) of late-stage hydrothermal fluids enriched in chalcophile Tl-Cu-Zn-Hg-As-Sb-S elements. Our study suggests that a complete series of ZnS–HgS solid solutions may be found in hydrothermal systems with a relatively high-temperature formation regime (>250 °C). In addition, Zn-Mn-bearing metacinnabar is a metastable phase in the Zn-Hg-Mn-S system. Mn is considered a stabilizer for metacinnabar, a natural counterpart of β-HgS, which is a prospective zero-gap semiconductor.

American MineralogistVol. 111(3)
St Petersburg University (RU), ORCID (US), Institute of Mineralogy (RU)
Openalex Percentile: Top 74%
Geological and Geochemical Analysis
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