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Cold springs of the Damxung Co basin

Central Tibet (Damxung Co basin), China

Groundwater

Type
Groundwater

DR-24 in Quaternary sediments of the central basin (31.539° N, 86.662° E), DR-34 in the northeast near bedrock (31.601° N, 86.792° E) and DR-60 in the southwest, downstream of the granite (31.432° N, 86.611° E); 8 to 9 °C. Water boron concentrations differ by a factor of about 8 between Table 2 (µg/L) and the text (mg/L), for every sample; the boron fluxes of Table 2 are consistent with the table values.

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
−9.9 ± 7.6 ‰−14.5 / −1.2 ‰3cold spring water
Mean and standard deviation recalculated from 3 analyses, -14.5 to -1.2 (DR-24 -14.1; DR-34 -14.5; DR-60 -1.2). DR-60, much heavier, is ascribed by the authors to a different host rock.
Lü et al. (2013), Origin of boron in the Damxung Co Salt Lake (central Tibet): Evidence f…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Cold springs of the Damxung Co basin, isotope signatures. https://www.isofind.tech/isotopes/en/sites/sources-froides-du-bassin-de-damxung-co/ (accessed 2026-10-20).

@misc{isofind2026coldspringsofthedamxungcobasi,
  title = {Cold springs of the Damxung Co basin, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/sources-froides-du-bassin-de-damxung-co/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20