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Takht-e Soleiman and Ahmadabad hot springs

West Azerbaijan Province, Takht-e Soleiman travertine-depositing geothermal field, Iran

Groundwater

Type
Groundwater

Hot springs (18 to 38 °C) of the travertine-depositing geothermal field, fed by meteoric water from the ranges hosting the Angouran deposit; a modern analogue of the hypogene smithsonite fluids. Indicative coordinates.

δ18O in ‰ (per mil) Values of the same system

Standard : V-SMOW

ValueRangenMineral or matrixSource
−10 ± 0.15 ‰−10.15 / −9.85 ‰3
Mean and standard deviation recalculated from 3 springs, Table 6.
Boni et al. (2007), Hypogene Zn carbonate ores in the Angouran deposit, NW Iran, Minerali…

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
−61 ± 0.7 ‰−61.5 / −60.2 ‰3
Mean and standard deviation recalculated from 3 springs, Table 6.
Boni et al. (2007), Hypogene Zn carbonate ores in the Angouran deposit, NW Iran, Minerali…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Takht-e Soleiman and Ahmadabad hot springs, isotope signatures. https://www.isofind.tech/isotopes/en/sites/sources-chaudes-de-takht-e-soleiman-et-d-ahmadabad/ (accessed 2026-10-13).

@misc{isofind2026takhtesoleimanandahmadabadhot,
  title = {Takht-e Soleiman and Ahmadabad hot springs, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/sources-chaudes-de-takht-e-soleiman-et-d-ahmadabad/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13