Permeability evolution during non-isothermal compaction in volcanic conduits and tuffisite veins: Implications for pressure monitoring of volcanic edifices

Journal: Earth and Planetary Science Letters

Published: 2019-12-01

DOI: 10.1016/j.epsl.2019.115783

Affiliations: 4

Authors: 3

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Institutions Share
Department of Earth, Ocean and Atmospheric Sciences (EOS), UBC, Canada 0.67
Department of Earth and Environmental Sciences, LMU, Germany 0.11
Department of Earth and Planetary Sciences (EPS), McGill University, Canada 0.11
Department of Geology, SUNY UB, United States of America (USA) 0.11

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