Sphalerite
Konaka, Azuma village, Midori city, Gunma pref., Japan
Source for Zinc, Cadmium, and Sulfuric acid.
Field of view: 10 mm. Sphalerite associated with rhodonite. The groups of transparent dark grayish-brown trapezohedrons are sphalerite. The surrounding transparent parts with a vitreous luster are quartz, and the transparent pink parts are rhodonite. The transparent pale brown parts at the upper left are spessartine.
Recovered from a chert-hosted bedded manganese deposit subjected to Hornblende-hornfels facies contact metamorphism by S-type (Ilmenite-series) granodiorite. Formed in the Late Cretaceous (90 Ma).
Sphalerite from this location was described in 1957.
Other localities
- Kamioka Mine (Pneumatolytic Skarn, Granular)
- Chichibu Mine (Hydrothermal Skarn, Twin)
- Nakatatsu Mine (Hydrothermal Skarn)
- Kawai Mine (Hydrothermal Skarn, Massive)
- Hagidaira Mine (Mn Skarn, Granular)
- Arakawa Mine (Hydrothermal, Transparent)
- Kawazu Mine (Hydrothermal, Granular)
- Mikawa Mine (Hydrothermal, Granular)
- Sayama Mine (Hydrothermal, Veinlet)
- Manju Mine (Hydrothermal, Massive)
- Hikida Mine (Hydrothermal, Granular)
- Agenosawa Mine (Hydrothermal, Massive)