Ca-metasomatism in the oceanic mantle as the result of high-T hydrothermal circulation: evidence from diopsidite dykes in the Oman ophiolite(abs.)

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

Ca-metasomatism in the oceanic mantle as the result of high-T hydrothermal circulation: evidence from diopsidite dykes in the Oman ophiolite(abs.)

Authors=PYTHON Marie, YOSHIKAWA Masako, SHIBATA Tomoyuki, CEULENEER Georges, ARAI Shoji

Journal/Book_names=Abstracts, 2011 Joint Annual Meeting of Japan Association of Mineralogical Sciences and the Geological Society of Japan (Section C)

volume=118

pages=61-61

Publish_year=2011

Publish_Country=JPN

Publisher=Geological Society of Japan, Japan Association of Mineralogical Sciences

Language_of_Text=EN

ISSN=13486543

ID=201122545

@id=https://gbank.gsj.jp/ld/resource/geolis/201122545