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Kyonosawa

Mitomi-Kamikamaguchi, Yamanashi city, Yamanashi pref., Japan

Occurrence

Acidic metasomatic rocks of Pyrophyllite zone

B-rich pyrophyllite deposit formed by hydrothermal alteration along the Sekisuiji fracture zone in the Konarayama Rhyolites (Konarayama volcanic rocks), a member of the early Pliocene (5.0 Ma) Higashi-Yamanashi Caldera. The Konarayama Rhyolites are composed of ryolitic-andesitic welded tuff, volcanic breccia, lava. The konarayama volcanic rocks unconformably overlies the Hirose granodiorite, and unconformably underlies the Yamaguchi pumice tuff of the Mizugamori volcanic rocks. The Sekisuiji fracture zone is a fault related to the Higashi-Yamanashi Caldera. The hydrothermal alteration was caused by the activity of the early Pleistocene (2.0 Ma) Mizugamori volcanic rocks. Ages of volcanic rocks were determined by K-Ar radiometric dating of whole rock and biotite. The type locality of magnesiofoitite.

Kyonosawa

Outcrop of andesite or dacite of the Konarayama Rhyolites subjected to pyrophyllitization alteration. White part is porous quartz, and dark green parts are veins of magnesiofoitite. Blue dumortierite is also included as spots.

Reported Minerals

  • Dumortierite
  • Magnesiofoitite
  • Pyrite
  • Sr-Natroalunite
  • Rutile
  • Muscovite

Mineral Assemblages

  • Quartz - Magnesiofoitite - Dumortierite - Muscovite
  • Quartz - Dumortierite
  • Andesite/Dacite(Host) - Pyrite

Localities

Related Occurrences

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