Ran Mangli mine (Nagpur)
Maharashtra, Nagpur district, India
Volcanogenic massive sulfidesCu
- Type
- Copper in metavolcanic rocks
Cu deposit of Early (?) Proterozoic age in a dominantly metavolcanic terrane, metamorphosed to greenschist facies. Palmer and Slack (1989, Table 2): tourmaline at -13.24 ‰. Tourmalines of this kind of terrane range from -15.71 to -1.49 ‰ 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 |
|---|---|---|---|---|
| −13.24 ‰ | 1 | tourmaline of the massive sulfide or associated tourmalinite Single analysis (T(RM)/6/89). Uncertainties: T(RM)/6/89 -13.24 ± 0.37 ‰. | Palmer & Slack (1989), Boron isotopic composition of tourmaline from massive sulfide depo… |
Deposits of the same type
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- Kidd Creek Canada
- Flin Flon Canada
- Rio Tinto Spain
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- Boliden Sweden
- Tharsis Spain
Cite this page
IsoFind Atlas (2026). Ran Mangli mine (Nagpur), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/mine-de-ran-mangli-nagpur/ (accessed 2026-10-19).
@misc{isofind2026ranmangliminenagpurisotopesig,
title = {Ran Mangli mine (Nagpur), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/mine-de-ran-mangli-nagpur/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19