Geological Literature Search (GEOLIS) (Geological Survey of Japan / AIST)

C-O-H fluid was present during garnet-forming partial melting reaction in a pelitic migmatite from the Ryoke belt, Japan (SMP25-06)(abs.)

Authors=Natsumi Yoshimoto, Tetsuo Kawakami

Journal/Book_names=Abstracts, Japan Geoscience Union Meeting (online)

volume=2021

pages=SMP25-06

Publish_year=2021

Publisher=Japan Geoscience Union

Language_of_Text=EN

ID=300021569

@id=https://gbank.gsj.jp/ld/resource/geolis/300021569