2025/09/18 by F. D. Sandalov, M.A. Rassomakhin, V. S. +4 · 1 voice
Computer Science · Earth and Planetary Sciences · Engineering · #Geochemistry and Geologic Mapping #Geological and Geochemical Analysis #Metal Extraction and Bioleaching
paper · doi:10.2138/am-2025-9783
openalex publication_date 2025/09/18 · openalex created_date 2025/10/10 · openalex updated_date 2026/06/11
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.