Sarylakh
Sakha (Yakutia), Russia
Epithermal depositsAu-Sb
- Type
- Mesothermal gold-quartz followed by epithermal stibnite
Taryn metallogenic zone in the Verkhoyansk-Kolyma belt, controlled by the Adycha-Taryn fault zone. Early milky-white quartz precipitated between 340 and 280 °C; later stibnite was deposited by remobilisation between 304 and 189 °C.
δ34S in ‰ (per mil) Values of the same system
Standard : V-CDT
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −2 / −0.9 ‰ | arsenopyrite Combined mesothermal and epithermal Au-Sb mineralisation. Three generations of stibnite (coarse, medium and fine grains) were analysed. | Bortnikov et al. 2010, Sarylakh and Sentachan gold-antimony deposits, Geology of Ore Depo… | ||
| −5.5 / −1.1 ‰ | pyrite | Bortnikov et al. 2010, Sarylakh and Sentachan gold-antimony deposits, Geology of Ore Depo… | ||
| −5.5 / −3.6 ‰ | stibnite | Bortnikov et al. 2010, Sarylakh and Sentachan gold-antimony deposits, Geology of Ore Depo… |
Deposits of the same type
- Sentachan Russia
- Zlatá Baňa Slovakia
- Kremnica Slovakia
- Matra France
- Cala Reona (Cartagena-Mazarrón district) Spain
- Hiendelaencina Spain
- Imiter Morocco
- Pueblo Viejo Dominican Republic
Cite this page
IsoFind Atlas (2026). Sarylakh, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/sarylakh/ (accessed 2026-10-06).
@misc{isofind2026sarylakhisotopesignatures,
title = {Sarylakh, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/sarylakh/},
note = {Accessed 2026-10-06}
}Updated : 2026-10-06