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Zawarmala

Rajasthan, Zawar belt (Aravalli Supergroup), India

Mississippi Valley TypePb-Zn

Type
Dolomite-hosted Pb-Zn

Deposit of the 20 km Zawar mineralized belt, in Palaeoproterozoic dolomites (about 1700 Ma) with phyllite intercalations, metamorphosed at greenschist facies (3 kbar, 400 to 450 °C). Classified SEDEX by some authors and MVT by others (Pb, carbonate host); Bhuyan et al. (2023) retain the MVT type. Syn-ore tourmaline from -6.6 to -4.0 ‰, boron from continental evaporites according to them.

δ11B in ‰ (per mil) Values of the same system

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−6.6 / −4 ‰10syn-ore tourmaline (Tur-I)
Range only. Schorl to dravite (XMg 0.22 to 0.67).
Bhuyan et al. (2023), Continental evaporites as brine sources for formation of SEDEX and …
−12.4 / −7.7 ‰13metamorphic tourmaline of phyllites (Tur-II)
Range only. Mg- and Na-rich.
Bhuyan et al. (2023), Continental evaporites as brine sources for formation of SEDEX and …

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Zawarmala, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/zawarmala/ (accessed 2026-10-20).

@misc{isofind2026zawarmalaisotopesignatures,
  title = {Zawarmala, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/zawarmala/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20