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Rhine at Kembs (placer, detrital Ru-Os-Ir alloys)

Haut-Rhin, Upper Rhine below Basel, France

Sediments

Type
Sediment

Detrital Ru-Os-Ir alloys from Upper Rhine gold and platinum-group mineral placers; Dijkstra et al. (2016) link them to Paleozoic residual peridotites of the Alps, accreted with the Armorican terranes before the Variscan orogeny. Over the four localities, main mode at 0.1244 (Re-depletion age 0.48 Ga) and inflection point at 0.1205 (1.06 Ga). Locality A of the appendix. Coordinates not published.

187Os/188Os isotope ratio, no unit Values of the same system

Standard : Rapport absolu, sans standard de référence

ValueRangenMineral or matrixSource
0.12455 ± 0.004130.11619 / 0.129488detrital Ru-Os-Ir alloys (single grains)
Mean and standard deviation recalculated from 8 analyses, 0.11619 to 0.12948 (AD Mt1 R91 0.11619; AD Mt1 R90 0.12199; AD Mt3 RK6 0.12407; AD Mt1 R87 0.12430; AD Mt1 R89 0.12533; AD Mt2 KK1 0.12705; AD Mt3 RK2 0.12796; AD Mt1 R93 0.12948). 2 suprachondritic grains (above 0.1276), which the authors attribute to mantle pyroxenites.
Dijkstra et al. (2016), Osmium isotope compositions of detrital Os-rich alloys from the R…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Rhine at Kembs (placer, detrital Ru-Os-Ir alloys), isotope signatures. https://www.isofind.tech/isotopes/en/sites/rhin-a-kembs-placer-alliages-ru-os-ir-detritiques/ (accessed 2026-10-20).

@misc{isofind2026rhineatkembsplacerdetritalruo,
  title = {Rhine at Kembs (placer, detrital Ru-Os-Ir alloys), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/rhin-a-kembs-placer-alliages-ru-os-ir-detritiques/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20