Camprafaud
Southern Massif Central (Montagne Noire), France
Other hydrothermalPb-Zn
- Type
- Pb-Zn vein
Late Hercynian vein in Lower Cambrian dolomites, on the overturned limb of a major recumbent fold. Indicative coordinates.
206Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 17.82 | 1 | galena One analysis, Table 2. Population 1, unradiogenic: syngenetic or diagenetic Cambrian mineralisation, or lead remobilised from such deposits. | Brevart et al. (1982), Metallogenic provinces and the remobilization process studied by l… |
207Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 15.6 | 1 | galena One analysis, Table 2. Population 1, unradiogenic: syngenetic or diagenetic Cambrian mineralisation, or lead remobilised from such deposits. | Brevart et al. (1982), Metallogenic provinces and the remobilization process studied by l… |
208Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 37.88 | 1 | galena One analysis, Table 2. Population 1, unradiogenic: syngenetic or diagenetic Cambrian mineralisation, or lead remobilised from such deposits. | Brevart et al. (1982), Metallogenic provinces and the remobilization process studied by l… |
Deposits of the same type
- Folat France
- Lacabarède France
- La Caunette France
- Argenneuves France
- Bournac France
- Lastours France
- Olargues France
- Berlou (Le Priou) France
Cite this page
IsoFind Atlas (2026). Camprafaud, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/camprafaud/ (accessed 2026-10-13).
@misc{isofind2026camprafaudisotopesignatures,
title = {Camprafaud, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/camprafaud/},
note = {Accessed 2026-10-13}
}Updated : 2026-10-13
