Melt Percolation, Melt-Rock Reaction and Oxygen Fugacity in Supra-Subduction Zone Mantle and Lower Crust from the Leka Ophiolite Complex, Norway (2021)
Attributed to:
Testing the 'wet versus dry' late veneer hypothesis
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1093/petrology/egab078
Publication URI: http://dx.doi.org/10.1093/petrology/egab078
Type: Journal Article/Review
Parent Publication: Journal of Petrology
Issue: 11