Eyller Bruch bog iron ore

Lower Rhine (North Rhine-Westphalia), Germany

OtherFe

Type
Bog iron ore (goethite)

Bog iron ore, formed by precipitation of dissolved groundwater iron in wet soils. Its iron composition varies widely between nodules and even within a nodule, which limits its use for provenance.

δ56Fe in ‰ (per mil) Values of the same system

Standard : IRMM-014

ValueRangenMineral or matrixSource
−0.19 ± 0.14 ‰−0.39 / 0.03 ‰7nodules and clays (Tote Rahm)
Mean and standard deviation of 7 analyses.
Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron …
−0.55 ± 0.35 ‰−1.29 / −0.09 ‰11nodules and crusts (Gelderner Fleuth)
Mean and standard deviation of 11 analyses.
Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron …
0.36 ± 0.49 ‰0.03 / 1.16 ‰5ore used for an experimental smelt
Mean and standard deviation of 5 analyses.
Rose et al. (2019), Questioning Fe isotopes as a provenance tool: Insights from bog iron …

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Eyller Bruch bog iron ore, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/minerai-de-fer-des-marais-d-eyller-bruch/ (accessed 2026-10-06).

@misc{isofind2026eyllerbruchbogironoreisotopes,
  title = {Eyller Bruch bog iron ore, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/minerai-de-fer-des-marais-d-eyller-bruch/},
  note = {Accessed 2026-10-06}
}

Updated : 2026-10-06