A Physical Model for Three‐Phase Compaction in Silicic Magma Reservoirs
Author:
Affiliation:
1. Department of Earth, Environmental and Planetary SciencesBrown University Providence RI USA
2. Department of Earth SciencesETH Zurich Zurich Switzerland
Funder
National Science Foundation
NSF CAREER
NSF EAR
Swiss National Funds
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017JB015224
Reference68 articles.
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4. On the Origin of Crystal-poor Rhyolites: Extracted from Batholithic Crystal Mushes
5. Gas percolation in upper-crustal silicic crystal mushes as a mechanism for upward heat advection and rejuvenation of near-solidus magma bodies
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