Depressed mantle discontinuities beneath Iceland: Evidence of a garnet controlled 660 km discontinuity? (2016)
Attributed to:
Interaction of Tectonics and Magmatism in the Askja spreading segment of Iceland
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.epsl.2015.10.053
Publication URI: http://dx.doi.org/10.1016/j.epsl.2015.10.053
Type: Journal Article/Review
Parent Publication: Earth and Planetary Science Letters