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.
Authors
- M.A. Rassomakhin (ORCID: https://orcid.org/0000-0001-8263-5525)
- Dmitry A. Artemyev (ORCID: https://orcid.org/0000-0003-1813-8932)
- Sergey N. Britvin (ORCID: https://orcid.org/0000-0003-3183-7594)
- V. S. (ORCID: https://orcid.org/0000-0002-2588-5322)
- F. D. Sandalov
- Е. В. Белогуб (ORCID: https://orcid.org/0000-0001-6623-3630)
- S. Yu. Stepanov (ORCID: https://orcid.org/0000-0002-5575-8906)
Institutions
- St Petersburg University (RU)
- ORCID (US)
- Institute of Mineralogy (RU)
Publication Details
- Journal
- American Mineralogist
- Published
- 2025-09-18
- DOI
- https://doi.org/10.2138/am-2025-9783
- Primary Topic
- Geological and Geochemical Analysis
- Type
- article
- Field-Weighted Citation Impact
- 0.00