Continuum approximation of dyking with a theory for poro-viscoelastic–viscoplastic deformation
Author:
Affiliation:
1. Department of Earth Sciences, University of Oxford , Oxford, OX1 3AN , UK
2. Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California San Diego , La Jolla, CA 92093 , USA
Abstract
Funder
European Research Council
National Science Foundation
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggad173/50064234/ggad173.pdf
Reference72 articles.
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2. High-resolution mapping of yield curve shape and evolution for high-porosity sandstone;Bedford;J. geophys. Res.,2019
3. How much magma is required to rift a continent?;Bialas;Earth planet. Sci. Lett.,2010
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