This shareable PDF can be hosted on any platform or network and is fully compliant with publisher copyright.
This publication has not yet been explained in plain language by the author(s). However, you can still read the publication.
If you are one of the authors, claim this publication so you can create a plain language summary to help more people find, understand and use it.
This page is a summary of: Temperature and strain-rate dependence of brittle rock deformation: Experimental study on Mohr-Coulomb’s failure criterion and Byerlee’s law for a low-porosity sandstone, September 2021, Society of Exploration Geophysicists,
DOI: 10.1190/segam2021-3583290.1.
You can read the full text:
Be the first to contribute to this page
