Doyashiki (Kannondo)
Akita Prefecture, Hokuroku district, Japan
Volcanogenic massive sulfidesZn-Pb-Cu (Ba)
- Type
- Kuroko-type volcanogenic massive sulfide
Kuroko-type massive sulfide deposit of the Hokuroku district, the type locality (Miocene). The ferruginous cherts (tetsusekiei) overlying the ores have widely scattered δ56Fe (-1.75 to +2.00 ‰ across the district), reflecting partial oxidation of hydrothermal iron in anoxic or suboxic pools; post-Kuroko ferruginous sediments range from -1.75 to +0.69 ‰, the youngest from -0.52 to +0.11 ‰. Indicative coordinates.
δ56Fe in ‰ (per mil) Values of the same system
Standard : IRMM-014
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −0.53 ± 0.58 ‰ | −1.57 / 0.03 ‰ | 10 | ferruginous chert and sediments (tetsusekiei) overlying the ore Mean and standard deviation recalculated from 10 samples, Supplementary Table 4. Bulk rock (microcrystalline hematite and quartz); variable Ce/Ce*. | Otake et al. (2021), Large Fe isotope fractionations in sulfide ores and ferruginous sedi… |
Deposits of the same type
- Matsumine Japan
- Ezuri Japan
- Fukazawa Japan
- Kosaka Japan
- Iheya North Mer de Chine orientale
- Iheya Ridge Mer de Chine orientale
- Tangyin Mer de Chine orientale
- Yonaguni IV Mer de Chine orientale
Cite this page
IsoFind Atlas (2026). Doyashiki (Kannondo), isotope signatures. https://www.isofind.tech/isotopes/en/deposits/doyashiki-kannondo/ (accessed 2026-10-13).
@misc{isofind2026doyashikikannondoisotopesigna,
title = {Doyashiki (Kannondo), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/deposits/doyashiki-kannondo/},
note = {Accessed 2026-10-13}
}Updated : 2026-10-13