The transition from porous to channelized flow due to melt/rock reaction during melt migration
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v021/i002/93GL03052/93GL03052.pdf
Reference17 articles.
1. Deformation of fine-grained aggregates of olivine plus melt at high temperatures and pressures;Beeman;J. Geophvs. Res.,1993
2. Reaction front fingering in carbonate cemented sandstones;Chen;Earth Science Reviews,1990
3. Rheology and structure of olivine-basalt partial melts;Cooper;J. Geophys. Res.,1986
4. A laboratory study of melt migration;Daines;Phil. Trans. R. Soc. Lond. A,1993
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