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Swaledale (Grinton Moor)

Yorkshire Dales (England), United Kingdom

Other hydrothermalPb-Zn

Type
Pb-Zn veins in Carboniferous limestones, oxidised near surface

Pb-Zn-F-Ba veins of the Askrigg Block; white and yellow-green smithsonite coatings around gossan material, the last layer Cd-rich. Sulfide oxidation at about 15 to 20 °C, under a climate warmer than today (Boni et al., 2019). Indicative coordinates.

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

Standard : V-SMOW

ValueRangenMineral or matrixSource
25.6 ± 0.4 ‰25.4 / 25.9 ‰2supergene smithsonite
Mean and standard deviation recalculated from 2 samples, Table 1. Specimens from the Natural History Museum (London) and private collections. One specimen located only as "Yorkshire".
Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu…

δ13C in ‰ (per mil) Values of the same system

Standard : V-PDB

ValueRangenMineral or matrixSource
−1.4 ± 0.7 ‰−1.9 / −0.9 ‰2supergene smithsonite
Mean and standard deviation recalculated from 2 samples, Table 1. Specimens from the Natural History Museum (London) and private collections. One specimen located only as "Yorkshire".
Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Swaledale (Grinton Moor), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/swaledale-grinton-moor/ (accessed 2026-10-13).

@misc{isofind2026swaledalegrintonmoorisotopesi,
  title = {Swaledale (Grinton Moor), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/swaledale-grinton-moor/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13