Compaction and Melt Transport in Ammonia-Rich Ice Shells: Implications for the Evolution of Triton
Author:
Affiliation:
1. Centre for Planetary Sciences; University of Toronto Scarborough; Toronto Ontario Canada
2. Department of Earth, Environmental and Planetary Sciences; Brown University; Providence RI USA
3. Planetary Science Institute; Tucson AZ USA
Funder
National Aeronautics and Space Administration
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018JE005781/fullpdf
Reference68 articles.
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2. Effective viscosity of partially melted ice in the ammonia-water system;Arakawa;Geophysical research letters,1994
3. Convection in ice I shells and mantles with self-consistent grain size;Barr;Journal of Geophysical Research,2007
4. The near infrared spectrum of MIranda: Evidence of crystalline water ice;Bauer;Icarus,2002
5. Composition gaps, critical crystallinity, and fractional crystallization in orogenic (calc-alkaline) magmatic systems;Brophy;Contributions to Mineralogy and Petrology,1991
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