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/10.17863/cam.55235
Publication URI: https://www.repository.cam.ac.uk/handle/1810/308141
Type: Journal Article/Review