Julcani
Huancavelica, central Peru, Peru
Epithermal depositsAg-Pb-Cu-Bi
- Type
- Polymetallic veins related to a volcanic centre
Central Andean mining district analysed for lead by Macfarlane et al. (1990); Late Miocene polymetallic veins in Miocene volcanics and Early Palaeozoic sediments (Excelsior Group). Coordinates from Table 2, to the nearest minute. Indicative coordinates.
206Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 18.545 ± 0.332 | 17.85 / 18.826 | 7 | galena from polymetallic veins Mean and standard deviation recalculated from 7 samples, Table 2 (PMP-70, 71, 72, 66, 67, 60 et 75). With Toquepala, one of only two deposits then known for significant internal lead variation; according to the authors, the largest internal variation of any deposit studied. Galena from veins hosted by phyllites and volcanics; PMP-66 (17.850) stands clearly apart. | Macfarlane et al. (1990), Lead isotope provinces of the Central Andes inferred from ores … |
207Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 15.666 ± 0.05 | 15.58 / 15.733 | 7 | galena from polymetallic veins Mean and standard deviation recalculated from 7 samples, Table 2 (PMP-70, 71, 72, 66, 67, 60 et 75). With Toquepala, one of only two deposits then known for significant internal lead variation; according to the authors, the largest internal variation of any deposit studied. Galena from veins hosted by phyllites and volcanics; PMP-66 (17.850) stands clearly apart. | Macfarlane et al. (1990), Lead isotope provinces of the Central Andes inferred from ores … |
208Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 38.659 ± 0.346 | 38.019 / 39.069 | 7 | galena from polymetallic veins Mean and standard deviation recalculated from 7 samples, Table 2 (PMP-70, 71, 72, 66, 67, 60 et 75). With Toquepala, one of only two deposits then known for significant internal lead variation; according to the authors, the largest internal variation of any deposit studied. Galena from veins hosted by phyllites and volcanics; PMP-66 (17.850) stands clearly apart. | Macfarlane et al. (1990), Lead isotope provinces of the Central Andes inferred from ores … |
Deposits of the same type
- Orcopampa Peru
- Quiruvilca Peru
- San José (Oruro) Bolivia
- Lavisa-Ocurí Bolivia
- Pulacayo Bolivia
- San Cristóbal (Nor Lípez) Bolivia
- Toldos (San Cristóbal district) Bolivia
- Pueblo Viejo Dominican Republic
Cite this page
IsoFind Atlas (2026). Julcani, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/julcani/ (accessed 2026-10-13).
@misc{isofind2026julcaniisotopesignatures,
title = {Julcani, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/julcani/},
note = {Accessed 2026-10-13}
}Updated : 2026-10-13
