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Montevecchio

Arbus and Guspini, south-western Sardinia, Italy

Other hydrothermalZn-Pb

Type
Variscan Pb-Zn veins around the Arbus granite

Large lead-zinc vein field of the Arburese, linked to the Variscan granite. Supergene smithsonite formed from meteoric waters at about 20 to 35 °C (Boni et al., 2003); light carbon inherited from soil and vegetation. Indicative coordinates.

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
20.7 ‰1Fe-rich smithsonite (monheimite)
One analysis, Table 1. Two analyses averaged; oxygen clearly lighter than in the Iglesiente.
Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i…

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

Standard : V-PDB

ValueRangenMineral or matrixSource
−4.98 ‰1Fe-rich smithsonite (monheimite)
One analysis, Table 1. Two analyses averaged; oxygen clearly lighter than in the Iglesiente.
Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Montevecchio, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/montevecchio/ (accessed 2026-10-13).

@misc{isofind2026montevecchioisotopesignatures,
  title = {Montevecchio, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/montevecchio/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13