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Kamojang geothermal field (Java)

Java, Indonesia

Other media

Type
Other medium

Geothermal systems of Java (Sunda arc) sampled in 2012-2013 by Purnomo et al. (2016); Quaternary volcanic systems receive magmatic fluids, fault-hosted systems in the south of the island mostly neutral waters. Coordinates not published (map only). Kendang volcanic complex.

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
2.3 ‰1hot spring water (dissolved boron)
Single analysis (J10 Kawah Hujan). 95.4 °C, pH 4.9, 4.63 mg/L B; steam separation from the B/Cl ratio.
Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,…
9.27 ‰1acid sulphate crater lake water (dissolved boron)
Single analysis (J9 Kawah Kamojang). 40 °C, pH 2.9, 1.39 mg/L B; 5.5 ‰ heavier than the Kawah Kreta vapour (evaporation and adsorption onto clays according to the authors).
Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,…
3.84 ‰1steam vent condensate (dissolved boron)
Single analysis (J73 Kawah Kreta). 3.49 mg/L B, chloride below detection; 3.8 ‰ heavier than the Dieng brines.
Purnomo et al. (2016), Boron isotope variations in geothermal systems on Java, Indonesia,…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Kamojang geothermal field (Java), isotope signatures. https://www.isofind.tech/isotopes/en/sites/champ-geothermal-de-kamojang-java/ (accessed 2026-10-19).

@misc{isofind2026kamojanggeothermalfieldjavais,
  title = {Kamojang geothermal field (Java), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/champ-geothermal-de-kamojang-java/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19