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Supplemental material: Origin of the dunitic mantle-crust transition zone in the Oman ophiolite: The interplay between percolating magmas and high-temperature hydrous fluids

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posted on 2017-01-01, 00:00 authored by M. Rospabé, et al.
GSA Data Repository Item 2017139, Geology.

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Origin of the dunitic mantle-crust transition zone in the Oman ophiolite: The interplay between percolating magmas and high-temperature hydrous fluids
GeologyGeology

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