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Springs at the margin of the Shihongtan uranium district

Xinjiang, southwestern margin of the Tuha (Turpan-Hami) basin, China

Groundwater

Type
Groundwater

Interlayer oxidation-zone sandstone uranium deposit, in sandstones of the Lower to Middle Jurassic Shuixigou Group; arid climate (17 mm rain per year, over 3000 mm evaporation). Groundwater flows from the southwest toward Aiting Lake. Min et al. (2007): meteoric waters, enriched along the flow path by water-rock interaction, evaporation and mixing with connate waters. Two springs from the confined parts of the aquifer: one in Quaternary gravels (fresh recharge water, facies 1), the other in Carboniferous volcaniclastic rocks. Without published coordinates.

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
1.5 ‰1spring water from Quaternary gravels (dissolved boron)
Single analysis (source 1). Fresh Na-Ca-HCO3 water, pH 7.0, 0.2 g/l TDS, 0.2 mg/l B.
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…
9.5 ‰1spring water from Carboniferous volcaniclastic rocks (dissolved boron)
Single analysis (source 2). pH 8.0, 17.2 g/l TDS, 1.3 mg/l B; strong interaction with volcanic rocks according to the authors.
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
−8.3 ‰1spring water from Quaternary gravels
Single analysis (source 1).
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…
−5.8 ‰1spring water from Carboniferous volcaniclastic rocks
Single analysis (source 2).
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
−48.2 ‰1spring water from Quaternary gravels
Single analysis (source 1).
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…
−43.4 ‰1spring water from Carboniferous volcaniclastic rocks
Single analysis (source 2).
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…

87Sr/86Sr isotope ratio, no unit Values of the same system

Standard : NIST SRM 987

ValueRangenMineral or matrixSource
0.706271spring water from Quaternary gravels (dissolved Sr)
Single analysis (source 1).
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…
0.709161spring water from Carboniferous volcaniclastic rocks (dissolved Sr)
Single analysis (source 2).
Min et al. (2007), Hydrochemistry and isotope compositions of groundwater from the Shihon…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Springs at the margin of the Shihongtan uranium district, isotope signatures. https://www.isofind.tech/isotopes/en/sites/sources-de-la-bordure-du-district-uranifere-de-shihongtan/ (accessed 2026-10-20).

@misc{isofind2026springsatthemarginoftheshihon,
  title = {Springs at the margin of the Shihongtan uranium district, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/sources-de-la-bordure-du-district-uranifere-de-shihongtan/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20