Matra

Haute-Corse (Alpine Corsica), France

Epithermal depositsAs (Sb)

Type
As (± Sb) epithermal, realgar and stibnite

A former arsenic mine with realgar and minor stibnite, in an Early Miocene brittle structure (Matra Fault). A high-temperature fluid (about 290 °C, 9 wt% NaCl equivalent) boiled at 500 to 800 m depth, then mixed with meteoric waters; a magmatic component linked to the opening of the Tyrrhenian Sea is likely.

δ13C in ‰ (per mil) Values of the same system

Standard : V-PDB

ValueRangenMineral or matrixSource
4.27 ‰4.1 / 4.5 ‰7first-generation dolomite
Samples MAT 10 and MAT 29 (main stage).
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
3.67 ‰3.6 / 3.7 ‰3second-generation dolomite (MAT 2)
Second generation, linked to reactivation of the Matra Fault.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
−0.43 ‰−0.5 / −0.4 ‰3second-generation dolomite (MAT 32)
Second generation, with lighter carbon.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
2.9 ‰2.8 / 3 ‰2calcite (MAT 23b)
Two analyses.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…

δ18O in ‰ (per mil) Values of the same system

Standard : V-PDB, V-SMOW

ValueRangenMineral or matrixSource
1.11 ‰0.4 / 1.6 ‰7first-generation dolomite
Samples MAT 10 and MAT 29 (main stage), δ18O relative to V-PDB.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
−3.8 ‰−4.4 / −3.4 ‰3second-generation dolomite (MAT 2)
δ18O relative to V-PDB.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
−0.93 ‰−1.1 / −0.7 ‰3second-generation dolomite (MAT 32)
δ18O relative to V-PDB.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
−2.2 ‰−2.8 / −1.6 ‰2calcite (MAT 23b)
δ18O relative to V-PDB.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…
4.3 / 10.6 ‰hydrothermal fluid (calculated water δ18O)
Values calculated for water in equilibrium with main-stage carbonates, not measured directly.
Filimon et al. (2026), Fluid sources and evolution in the As (±Sb) epithermal Matra depos…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Matra, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/matra/ (accessed 2026-10-06).

@misc{isofind2026matraisotopesignatures,
  title = {Matra, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/matra/},
  note = {Accessed 2026-10-06}
}

Updated : 2026-10-06