Mineville
New York, eastern Adirondacks, United States
IOCGFe
- Type
- Iron oxide-apatite (Kiruna type)
Strongly altered iron oxide-apatite deposit, considered by Bilenker et al. (2016) to have formed by secondary hydrothermal activity: magnetite δ56Fe (-0.92 ‰) and δ18O (-0.79 ‰) outside the magmatic range, unlike the Chilean deposits. Indicative coordinates (Mineville township).
δ56Fe in ‰ (per mil) Values of the same system
Standard : IRMM-014
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.92 ± 0.03 ‰ | 1 | altered massive magnetite Single analysis; 2σ uncertainty; negative sign checked on the image (lost in the extracted text, which gives +0.92 ‰). | Bilenker et al. (2016), Fe–O stable isotope pairs elucidate a high-temperature origin of … |
δ18O in ‰ (per mil) Values of the same system
Standard : V-SMOW
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.79 ± 0.03 ‰ | 1 | altered massive magnetite Single analysis; 2σ uncertainty; negative sign checked on the image. | Bilenker et al. (2016), Fe–O stable isotope pairs elucidate a high-temperature origin of … |
Deposits of the same type
- Alvo 118 Brazil
- Castanha Brazil
- Sossego Brazil
- Bacaba Brazil
- El Laco Chile
- Quince Chile
- Candelaria-Punta del Cobre district Chile
- Los Colorados Chile
Cite this page
IsoFind Atlas (2026). Mineville, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/mineville/ (accessed 2026-10-15).
@misc{isofind2026minevilleisotopesignatures,
title = {Mineville, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/mineville/},
note = {Accessed 2026-10-15}
}Updated : 2026-10-15