Crystallographic Preferred Orientation of Olivine in Sheared Partially Molten Rocks: The Source of the "a-c Switch" (2018)
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/10.1002/2017gc007309
Publication URI: http://dx.doi.org/10.1002/2017gc007309
Type: Journal Article/Review
Parent Publication: Geochemistry, Geophysics, Geosystems
Issue: 2