Olivine-quartz association in a gabbro-peridotite hybrid rock of the Kane Fracture Zone: evidence for hydrous Si-rich melt percolation in abyssal context.

Bickert, Manon; Rospabé, Mathieu; Kaczmarek, Mary-Alix; Maia, Marcia

doi:10.5194/egusphere-egu25-11050

Olivine-quartz association in a gabbro-peridotite hybrid rock of the Kane Fracture Zone: evidence for hydrous Si-rich melt percolation in abyssal context.

Full Text

File	Pages	Size	Access
Résumé	2	307 Ko		Download

How to cite

Bickert Manon, Rospabé Mathieu, Kaczmarek Mary-Alix, Maia Marcia (2025). Olivine-quartz association in a gabbro-peridotite hybrid rock of the Kane Fracture Zone: evidence for hydrous Si-rich melt percolation in abyssal context. EGU General Assembly 2025. 27 Apr–2 May 2025, Vienna, Austria. https://doi.org/10.5194/egusphere-egu25-11050, https://archimer.ifremer.fr/doc/00944/105616/

Copy this text