Gorob prospect (Namibia)
Damara belt (Matchless), Namibia
Volcanogenic massive sulfidesCu-Zn
- Type
- Besshi-type massive sulfides (Cu-Zn) in metasediments
Cu-Zn deposit of Late Proterozoic age in a dominantly clastic metasedimentary terrane, metamorphosed to amphibolite facies. Palmer and Slack (1989, Table 1): tourmaline at -8.14 ‰. Tourmalines of this kind of terrane range from -15.37 to -2.19 ‰ in the article; according to the authors, the boron source (continental crust, entrained seawater, evaporites) matters more than the formation temperature.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −8.14 ‰ | 1 | tourmaline of the massive sulfide or associated tourmalinite Single analysis (HP-388). Uncertainties: HP-388 -8.14 ± 0.36 ‰. | Palmer & Slack (1989), Boron isotopic composition of tourmaline from massive sulfide depo… |
Deposits of the same type
- Iberian Pyrite Belt (representative example) Spain/Portugal
- Neves-Corvo Portugal
- Kidd Creek Canada
- Flin Flon Canada
- Rio Tinto Spain
- Cyclades (Kondaros-Katsimouti and Triades) Greece
- Boliden Sweden
- Tharsis Spain
Cite this page
IsoFind Atlas (2026). Gorob prospect (Namibia), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/prospect-de-gorob-namibie/ (accessed 2026-10-19).
@misc{isofind2026gorobprospectnamibiaisotopesi,
title = {Gorob prospect (Namibia), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/prospect-de-gorob-namibie/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19