The transition from porous to channelized flow due to melt/rock reaction during melt migration
- 15 January 1994
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 21 (2) , 145-148
- https://doi.org/10.1029/93gl03052
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- Pacific lower crustal and shallow mantle sections recoveredEos, 1993
- Deformation of fine‐grained aggregates of olivine plus melt at high temperatures and pressuresJournal of Geophysical Research, 1993
- A laboratory study of melt migrationPhilosophical Transactions A, 1993
- Kinetics of melt migration in upper mantle-type rocksEarth and Planetary Science Letters, 1991
- Reaction front fingering in carbonate-cemented sandstonesEarth-Science Reviews, 1990
- Reaction Between Ultramafic Rock and Fractionating Basaltic Magma I. Phase Relations, the Origin of Calc-alkaline Magma Series, and the Formation of Discordant DuniteJournal of Petrology, 1990
- Pore evolution and channel formation during flow and reaction in porous mediaAIChE Journal, 1988
- Geochemical self-organization II; the reactive-infiltration instabilityAmerican Journal of Science, 1987
- Rheology and structure of olivine‐basalt partial meltsJournal of Geophysical Research, 1986
- The origin and significance of large, tabular dunite bodies in the Trinity peridotite, northern CaliforniaContributions to Mineralogy and Petrology, 1982