Hematite
Higashi-Akatani, Shibata city, Niigata pref., Japan
Source for Iron
Field of view: 50 mm. Groups of hematite. The radial groups of black platy crystals are hematite. The reddish-brown host is metamorphosed limestone containing fine hematite grains.
Recovered from a moderate temperature hydrothermal deposit associated with an oxidative metazomatic zone combined with skarn formed by contact metamorphism of S-type (Ilmenite-series) granodiorite. Formed in the early Miocene (21 Ma).
Hematite from this location was described in 1893.
Other localities
- Waga-sennin Mine (Metasomatic Skarn, Rosette)
- Akatani Mine (Metasomatic Skarn, Platy)
- Chichibu Mine (Hydrothermal Skarn, Platy)
- Mikawa Mine (Hydrothermal, Botryoidal)
- Gozaisho Mine (Bedded Mn, Tabular)
- Iwaisawa Mine (Bedded Mn, Massive)
- Sukayu (Bog Iron, Powder)
- Gunma Mine (Bog Iron, Powder)