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Narayani (Gandak, Nepal)

Nepal, Lesser Himalaya and plain, Népal

Rivers and surface water

Type
River or surface water

River formed by the junction of the Kali Gandaki and the Trisuli in the Lesser Himalaya (schists and quartzites, minor limestones). Without published coordinates.

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

Standard : NIST SRM 951

ValueRangenMineral or matrixSource
9 ± 4.6 ‰3.5 / 14.2 ‰4filtered river water (dissolved boron)
Mean and standard deviation recalculated from 4 analyses, +3.5 to +14.2 (NH1 +14.2; NAG49 +7.2; LO308 +10.9; MO215 +3.5). Elevation, dissolved B and 1σ uncertainty: NH1: 225 m, 2.41 µmol/l, ± 0.9 ‰; NAG49: 190 m, 1.20 µmol/l, ± 1.9 ‰; LO308: 305 m, 0.74 µmol/l, ± 1.5 ‰; MO215: 220 m, 1.67 µmol/l, ± 0.6 ‰.
Rose et al. (2000), Fractionation of boron isotopes during erosion processes: the example…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Narayani (Gandak, Nepal), isotope signatures. https://www.isofind.tech/isotopes/en/sites/narayani-gandak-nepal/ (accessed 2026-10-20).

@misc{isofind2026narayanigandaknepalisotopesig,
  title = {Narayani (Gandak, Nepal), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/narayani-gandak-nepal/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20