@article{oai:kanazawa-u.repo.nii.ac.jp:00010101,
 author = {石渡, 明 and 辻森, 樹 and 仁科, 克一 and 板谷, 徹丸},
 issue = {9},
 journal = {地質学雑誌},
 month = {Sep},
 note = {The Fuko Pass metacumulate is a tectonic block (4.5×1.5 km in size) within the Oeyama peridotite body in the Inner Zone of southwestern Japan. It was metamorphosed under the high-pressure and moderate-temperature condition to form a mineral assemblage hornblende+clinozoisite+kyanite+paragonite+albite+rutile. K-Ar ages were determined on hornblende separates from four epidote amphibolite samples, yielding 443-403 Ma. This suggests a Siluro-Ordovician subduction-related metamorphic event for the Fuko Pass metacumulate, which is distinct from the Late Paleozoic high-P/T type metamorphic events of the Renge metamorphic belt in the Inner Zone of southwestern Japan. The Fuko Pass metacumulate is correlated, in age, with the Early Paleozoic high-P/T type schists (445-402 Ma) of the Kurosegawa klippe in the Outer Zone., 金沢大学大学院自然科学研究科},
 pages = {646--649},
 title = {西南日本内帯大江山地域の普甲峠変成沈積岩に産する4～4.4億年含藍晶石緑れん石角閃岩},
 volume = {106},
 year = {2000}
}