On the Origin of Radial Anisotropy Near Subducted Slabs in the Midmantle (2019)
Attributed to:
Origin of seismic heterogeneity and attenuation in the Earth's upper mantle and transition zone
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2019gc008462
Publication URI: http://dx.doi.org/10.1029/2019gc008462
Type: Journal Article/Review
Parent Publication: Geochemistry, Geophysics, Geosystems
Issue: 11