Kremnica
Western Carpathians, Slovakia
Epithermal depositsAu-Ag (Sb associe)
- Type
- Low-sulfidation epithermal
Hosted in a Neogene volcanic field. Stibnite-rich veins occur outside the main vein structures, with illite, illite-smectite and kaolinite alteration. Late fluids were of low salinity (below 2 wt% NaCl equivalent) and low temperature (below 150 °C).
δ123Sb in ‰ (per mil) Values of the same system
Standard : NIST SRM 3102a
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.15 / 1.28 ‰ | stibnite Molar mS/mSb ratio of about 3 to 4 at Kremnica. Progressive Rayleigh fractionation coupling Sb and S, with mineralisation by mixing of an acidic, CO2-rich fluid at the margin of the epithermal system. | Kodera et al. 2024, Coupled antimony and sulfur isotopic composition of stibnite, Kremnic… |
Deposits of the same type
- Zlatá Baňa Slovakia
- Matra France
- Cala Reona (Cartagena-Mazarrón district) Spain
- Hiendelaencina Spain
- Imiter Morocco
- Pueblo Viejo Dominican Republic
- San José (Oruro) Bolivia
- Sarylakh Russia
Cite this page
IsoFind Atlas (2026). Kremnica, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/kremnica/ (accessed 2026-10-06).
@misc{isofind2026kremnicaisotopesignatures,
title = {Kremnica, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/kremnica/},
note = {Accessed 2026-10-06}
}Updated : 2026-10-06