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Kunimiyama

Central Shikoku, Northern Chichibu Belt (Sumaizuku Unit), Japan

OtherFe-Mn

Type
Hydrothermal-hydrogenetic ferromanganese umber on mid-ocean ridge basalt, within an accretionary complex

Early Permian umber (Sakmarian, 293.5 to 290.5 Ma) at the contact between mid-ocean ridge basalt and red chert, in the ocean plate stratigraphy of the Sumaizuku Unit; Anagawa, Asahi, Kagami (the largest, 4 m thick on average and up to 12 m), Akatsuki and Noboru ore bodies. Hematite-dominated ore with minor caryopilite and calcite veinlets. Mined from 1941 to 1961, about 0.12 Mt of ore at 25-30 % Fe and 15-25 % Mn; samples taken from mine dumps. Prehnite-pumpellyite facies metamorphism.

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

Standard : Rapport absolu, sans standard de référence

ValueRangenMineral or matrixSource
0.6235 ± 0.04650.5463 / 0.67586umber (bulk), Kagami ore body, initial ratio (187Os/188Os)i at 292 Ma
Mean and standard deviation recalculated from 6 analyses, 0.5463 to 0.6758 (04ku076 0.5463; 04ku078 0.6246; 04ku080 0.6653; 04ku081 0.6246; 04ku085 0.6046; 04ku150 0.6758). Initial ratios recalculated by the authors at 292.015 Ma (mid-Sakmarian). Duplicates averaged: 04ku081 0.6257 and 0.6234.
Yano et al. (2023), Marine osmium isotopic composition reconstructed from the early Permi…
0.6027 ± 0.04160.5228 / 0.648411umber (bulk), Noboru ore body, initial ratio (187Os/188Os)i at 292 Ma
Mean and standard deviation recalculated from 11 analyses, 0.5228 to 0.6484 (04ku120 0.5904; 04ku121 0.5835; 04ku122 0.6484; 04ku123 0.6358; 04ku124 0.6143; 04ku125 0.6353; 04ku126 0.5804; 04ku127 0.6410; 04ku128 0.5464; 04ku129 0.5228; 04ku130 0.6318). Initial ratios recalculated by the authors at 292.015 Ma (mid-Sakmarian). Duplicates averaged: 04ku127 0.6230 and 0.6590. 04ku127 and 04ku128 carry 44 to 49 ppt Re, against 1.3 to 14 ppt elsewhere.
Yano et al. (2023), Marine osmium isotopic composition reconstructed from the early Permi…
0.6038 ± 0.02640.5787 / 0.64375umber (bulk), Akatsuki ore body, initial ratio (187Os/188Os)i at 292 Ma
Mean and standard deviation recalculated from 5 analyses, 0.5787 to 0.6437 (04ku138 0.5995; 04ku139 0.6437; 04ku140 0.5827; 04ku141 0.5787; 04ku142 0.6143). Initial ratios recalculated by the authors at 292.015 Ma (mid-Sakmarian). Duplicates averaged: 04ku140 0.5834 and 0.5819. The table spells "Akatusuki".
Yano et al. (2023), Marine osmium isotopic composition reconstructed from the early Permi…
0.6114 ± 0.03920.5239 / 0.676822umber (bulk), measured present-day ratio
Mean and standard deviation recalculated from 22 analyses, 0.5239 to 0.6768 (04ku076 0.5466; 04ku078 0.6255; 04ku080 0.6659; 04ku081 0.6251; 04ku085 0.6049; 04ku150 0.6768; 04ku120 0.5915; 04ku121 0.5849; 04ku122 0.6506; 04ku123 0.6371; 04ku124 0.6156; 04ku125 0.6368; 04ku126 0.5813; 04ku127 0.6542; 04ku128 0.5619; 04ku129 0.5239; 04ku130 0.6341; 04ku138 0.6014; 04ku139 0.6457; 04ku140 0.5862; 04ku141 0.5791; 04ku142 0.6214). 22 samples from the Kagami, Noboru and Akatsuki ore bodies, duplicates averaged. Os 42 to 183 ppt, Re 1.3 to 49 ppt, 187Re/188Os 0.06 to 3.2: the age correction stays small, and the published mean initial ratio is 0.608 ± 0.039 (1 SD). The authors read it as early Permian seawater, Os being mostly hydrogenetic. Duplicates of 04ku127: 0.6357 and 0.6727 (initial 0.6230 and 0.6590), far beyond the 2 SE (0.0012 to 0.0014). Duplicates of 04ku140: 187Re/188Os of 0.988 and 0.450 for almost identical Re and Os contents (6.51 and 6.23 ppt; 70.60 and 70.69 ppt), which suggests an error in the table.
Yano et al. (2023), Marine osmium isotopic composition reconstructed from the early Permi…

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Cite this page

IsoFind Atlas (2026). Kunimiyama, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/kunimiyama/ (accessed 2026-10-20).

@misc{isofind2026kunimiyamaisotopesignatures,
  title = {Kunimiyama, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/kunimiyama/},
  note = {Accessed 2026-10-20}
}

Updated : 2026-10-20