Variability of protoliths and pressure-temperature conditions of amphibolites from the Ohmachi Seamount (Izu-Bonin-Mariana arc): evidence of a fossil subduction channel in a modern intra-oceanic arc
Crossref DOI link: https://doi.org/10.1007/s00710-020-00705-z
Published Online: 2020-05-23
Published Print: 2020-08
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Imayama, Takeshi
Ueda, Hayato
Usuki, Tadashi
Minami, Masayo
Asahara, Yoshihiro
Nagahashi, Toru
Text and Data Mining valid from 2020-05-23
Version of Record valid from 2020-05-23
Article History
Received: 27 January 2019
Revised: 8 March 2020
Accepted: 24 March 2020
First Online: 23 May 2020