Olivine anisotropy suggests Gutenberg discontinuity is not the base of the lithosphere. (2016)
Attributed to:
A new method for mapping stresses in mantle rocks: Dislocation density from electron-backscatter diffraction
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1073/pnas.1608269113
PubMed Identifier: 27606485
Publication URI: http://europepmc.org/abstract/MED/27606485
Type: Journal Article/Review
Volume: 113
Parent Publication: Proceedings of the National Academy of Sciences of the United States of America
Issue: 38
ISSN: 0027-8424