Kolar
Karnataka, India
Orogenic goldAu (W)
- Type
- Gold-scheelite quartz veins in a greenstone belt
Historic gold field in the Archean Kolar greenstone belt (mineralisation about 2.4 Ga), one of the deepest gold mines in the world. Indicative coordinates.
206Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 14.446 | 1 | scheelite One analysis, Table 2. Measured ratios, not age-corrected: the author regards them as close to initial common lead. | Chiaradia (2003), The evolution of tungsten sources in crustal mineralization from Archea… |
207Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 14.972 | 1 | scheelite One analysis, Table 2. Measured ratios, not age-corrected: the author regards them as close to initial common lead. | Chiaradia (2003), The evolution of tungsten sources in crustal mineralization from Archea… |
208Pb/204Pb isotope ratio, no unit Values of the same system
Standard : NIST SRM 981
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 33.866 | 1 | scheelite One analysis, Table 2. Measured ratios, not age-corrected: the author regards them as close to initial common lead. | Chiaradia (2003), The evolution of tungsten sources in crustal mineralization from Archea… |
Deposits of the same type
- Guoluolongwa China
- Muruntau Uzbekistan
- Daugyztau Uzbekistan
- Baguamiao China
- Berezovsk (Berezovskoye) Russia
- Kalgoorlie (Golden Mile) Australia
- Golden Mile (Kalgoorlie) Australia
- Schellgaden Austria
Cite this page
IsoFind Atlas (2026). Kolar, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/kolar/ (accessed 2026-10-13).
@misc{isofind2026kolarisotopesignatures,
title = {Kolar, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/kolar/},
note = {Accessed 2026-10-13}
}Updated : 2026-10-13
