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Sadisdorf

Eastern Erzgebirge, Saxony, Germany

Other hydrothermalSn-W-Li

Type
Tin greisen and breccia

Greisenised tin-tungsten-lithium granite cupola of the eastern Erzgebirge (Late Carboniferous). Indicative coordinates.

δ124Sn in ‰ (per mil) Values of the same system

Standard : NIST SRM 3161a

ValueRangenMineral or matrixSource
0.46 ‰1cassiterite
One analysis, Table 2. Ore age used by the authors: 320 Ma.
Mathur et al. (2025), Global Sn isotope compositions of cassiterite identify the magmatic…

206Pb/204Pb isotope ratio, no unit Values of the same system

Standard : NIST SRM 981

ValueRangenMineral or matrixSource
18.597 ± 0.26818.241 / 18.8834sulfide ore (ore minerals hand-picked)
Mean and standard deviation recalculated from 4 samples, Table 5 (99, 218, 219 et 221: arsenopyrite, chalcopyrite and molybdenite; fahlore; chalcopyrite and cassiterite; chalcopyrite, cassiterite and emplectite (Kupfergrube mine)). Strong scatter due to radiogenic lead from a superimposed late or post-Variscan uranium mineralisation, common in the Erzgebirge according to the authors.
Niederschlag et al. (2003), The determination of lead isotope ratios by multiple collecto…

207Pb/204Pb isotope ratio, no unit Values of the same system

Standard : NIST SRM 981

ValueRangenMineral or matrixSource
15.625 ± 0.01915.598 / 15.6424sulfide ore (ore minerals hand-picked)
Mean and standard deviation recalculated from 4 samples, Table 5 (99, 218, 219 et 221: arsenopyrite, chalcopyrite and molybdenite; fahlore; chalcopyrite and cassiterite; chalcopyrite, cassiterite and emplectite (Kupfergrube mine)). Strong scatter due to radiogenic lead from a superimposed late or post-Variscan uranium mineralisation, common in the Erzgebirge according to the authors.
Niederschlag et al. (2003), The determination of lead isotope ratios by multiple collecto…

208Pb/204Pb isotope ratio, no unit Values of the same system

Standard : NIST SRM 981

ValueRangenMineral or matrixSource
38.523 ± 0.29138.17 / 38.884sulfide ore (ore minerals hand-picked)
Mean and standard deviation recalculated from 4 samples, Table 5 (99, 218, 219 et 221: arsenopyrite, chalcopyrite and molybdenite; fahlore; chalcopyrite and cassiterite; chalcopyrite, cassiterite and emplectite (Kupfergrube mine)). Strong scatter due to radiogenic lead from a superimposed late or post-Variscan uranium mineralisation, common in the Erzgebirge according to the authors.
Niederschlag et al. (2003), The determination of lead isotope ratios by multiple collecto…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Sadisdorf, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/sadisdorf/ (accessed 2026-10-13).

@misc{isofind2026sadisdorfisotopesignatures,
  title = {Sadisdorf, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/sadisdorf/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13