Controls on the rheological properties of peridotite at a palaeosubduction interface: A transect across the base of the Oman-UAE ophiolite (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.53234
Publication URI: https://www.repository.cam.ac.uk/handle/1810/306154
Type: Journal Article/Review