Melting and Evolution of Amphibole‐Rich Back‐Arc Abyssal Peridotites at the Mado Megamullion, Shikoku Basin

Abstract The Mado Megamullion is an oceanic core complex (OCC) in the Shikoku back‐arc basin within the Philippine Sea Plate. Mantle peridotites (serpentinized) recovered by six dredge and submersible cruises exhibit signatures of extensive deformation. Amorphous pseudomorphs after plagioclase in ma...

תיאור מלא

מידע ביבליוגרפי
Main Authors: A. Sen, J. E. Snow, Y. Ohara, K. Hirauchi, Y. Kouketsu, A. Sanfilippo, V. Basch, Y. Harigane, M. Fujii, K. Okino, N. Akizawa
פורמט: Article
שפה:English
יצא לאור: Wiley 2021-12-01
סדרה:Geochemistry, Geophysics, Geosystems
נושאים:
גישה מקוונת:https://doi.org/10.1029/2021GC010013