Ref.: Geological Survey of Japan (1960).
Shiga, Y. (1987) Behavior of iron, nickel, cobalt and sulfur during serpentinization, with reference to Hayachine ultramafic rocks of the Kamaishi mining district, northeastern Japan. Canadian Mineralogist: 25: 611-624.
Anthony, Bideaux, Bladh, Nichols: "Handbook of Mineralogy", Vol. 1, 1990;
Rocks & Minerals: 22: 320.
An abandoned iron-copper mine at least 500 meters deep. Contact metasomatic (skarn) ores around a Cretaceous dioritic granite intrusion. Worked for iron (magnetite orebodies) and copper-gold-silver (chalcopyrite-cubanite orebodies). At least 15 orebodies, including Shinyama, Nippo, Sahinai and Rasa-Omine orebodies. Shinyama is the largest Fe skarn orebody in Japan, 400m long, 80m wide, 550m high. Magnetite-garnet skarns were worked for iron already during the Tokugawa shogunate era, with Japan's first modern blast furnace built here in 1857 (late Edo era). Peak production was in the 1970s. 1958 production: 1.04 million tons ore averaging 28.6% Fe (the highest Fe ore production in Japan). Mine now closed, but there is commercial production of bottled mineral water.
