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High-B geothermal springs of southern Tibet (Buxionglanggu, Shagalangga, Babudemi, Chaka, Lawangzi)

Tibet (Xizang), China

Other media

Type
Other medium

Geothermal waters of the Tibetan Plateau sampled by Zhang et al. (2015): high-B waters (36.8 to 171.9 mg/L, Na-Cl, mostly 85-87 °C) along the Indus-Yarlung Zangbo suture and the N-S rifts, magmatic boron supplied by degassing of a cooling magma; low-B waters (0.4 to 34.6 mg/L, Na-Ca-HCO3-SO4) of the Lhasa block, boron leached from host rocks by water-rock interaction. Coordinates not published (map only). Na-Cl waters at 38 to 87 °C, 121.3 to 171.9 mg/L B, lowest Cl/B ratios (magmatic degassing).

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−11.27 ± 0.65 ‰−12.43 / −10.87 ‰5geothermal water (dissolved boron)
Mean and standard deviation recalculated from 5 analyses, -12.43 to -10.87 (Buxionglanggu -10.87; Shagalangga -10.97; Babudemi -11.02; Chaka -11.08; Lawangzi -12.43).
Zhang et al. (2015), Boron geochemistry from some typical Tibetan hydrothermal systems: O…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). High-B geothermal springs of southern Tibet (Buxionglanggu, Shagalangga, Babudemi, Chaka, Lawangzi), isotope signatures. https://www.isofind.tech/isotopes/en/sites/sources-geothermales-a-bore-eleve-du-tibet-meridional-buxionglanggu-shagalangga-babudemi-chaka-lawangzi/ (accessed 2026-10-19).

@misc{isofind2026highbgeothermalspringsofsouth,
  title = {High-B geothermal springs of southern Tibet (Buxionglanggu, Shagalangga, Babudemi, Chaka, Lawangzi), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/sources-geothermales-a-bore-eleve-du-tibet-meridional-buxionglanggu-shagalangga-babudemi-chaka-lawangzi/},
  note = {Accessed 2026-10-19}
}

Updated : 2026-10-19