2017139_SupplementaryData.xlsx (78.17 kB)
Supplemental material: Origin of the dunitic mantle-crust transition zone in the Oman ophiolite: The interplay between percolating magmas and high-temperature hydrous fluids
journal contribution
posted on 2017-01-01, 00:00 authored by M. Rospabé, et al.GSA Data Repository Item 2017139, Geology.
