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Puga geothermal field (Ladakh)

Ladakh, Puga valley, India

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Type
Other medium

Geothermal field just south of the Indus Suture Zone, at about 4400 m elevation (boiling near 84.5 °C), over 5 km long, with mud pools, hot springs, siliceous sinters and borate crusts (tincalconite). Steller et al. (2019): homogeneous fluids near -12.7 ‰ (126 to 138 ppm B); solids from -14.3 to -41.0 ‰, fractionation coming from tetrahedral borate uptake into amorphous silica rather than evaporation. Indicative coordinates, not published in the article.

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−12.7 ± 0.3 ‰−13.1 / −12.2 ‰6hot-spring geothermal fluid (dissolved boron)
Mean and standard deviation recalculated from 6 analyses, -13.1 to -12.2 (PU_01F -12.2; PU_07F -12.8; PU_09F -13.1; PU_10F -12.7; PU_11F -12.8; PU_14F -12.5). 26 to 84.5 °C, pH 6.3 to 7.8, 126 to 138 ppm B. The authors give a -12.6 ‰ mean.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…
−12.8 ‰1mud-pool pore water (filtered)
Single analysis (PU_07BF). 25 °C, pH 5.9, 440 ppm B.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…
−14.4 ± 0.1 ‰−14.5 / −14.3 ‰2evaporitic crusts and pastes (halite, tincalconite)
Mean and standard deviation recalculated from 2 analyses, -14.5 to -14.3 (PU_05S -14.5; PU_10S -14.3). PU_05S: halite-sulfur paste, 13,700 ppm B; PU_10S: puffy tincalconite crust, 99,700 ppm B, representative of large areas of the field.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…
−17.6 ‰1mud-pool rim sediment (muscovite, sulfur)
Single analysis (PU_07AS). 2620 ppm B.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…
−36 ± 2.6 ‰−37.8 / −34.1 ‰2siliceous sinter (laminated crust and digitate nodules of amorphous silica)
Mean and standard deviation recalculated from 2 analyses, -37.8 to -34.1 (PU_11AS -34.1; PU_14S -37.8). PU_11AS: laminated amorphous silica and quartz crust with filaments, 4210 ppm B; PU_14S: amorphous silica and calcite nodules on an outflow terrace, 6380 ppm B.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…
−28.3 ‰1hot-spring sediment (quartz, muscovite, calcite)
Single analysis (PU_11BS). 2490 ppm B.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…
−41 ‰1diatom-rich suspended sediment (mud pool)
Single analysis (PU_07BR). 441 ppm B; lowest non-coal value according to the authors.
Steller et al. (2019), Boron isotopes in the Puga geothermal system, India, and their imp…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Puga geothermal field (Ladakh), isotope signatures. https://www.isofind.tech/isotopes/en/sites/champ-geothermal-de-puga-ladakh/ (accessed 2026-10-19).

@misc{isofind2026pugageothermalfieldladakhisot,
  title = {Puga geothermal field (Ladakh), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/champ-geothermal-de-puga-ladakh/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19