A dynamic model for generating small‐scale heterogeneities in ocean floor basalts
- 10 June 1995
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 100 (B6) , 10141-10162
- https://doi.org/10.1029/94jb03102
Abstract
No abstract availableKeywords
This publication has 125 references indexed in Scilit:
- Compositional variation in a steady-state zoned magma chamber: Mid-Atlantic Ridge at 36°50′NPublished by Elsevier ,2003
- Solution-precipitation enhanced diffusional creep of partially molten olivine-basalt aggregates during hot-pressingPublished by Elsevier ,2003
- Focused mantle upwelling beneath mid-ocean ridges: evidence from seamount formation and isostatic compensation of topographyEarth and Planetary Science Letters, 1992
- Melt migration in a silicate liquid‐olivine system: An experimental test of compaction theoryGeophysical Research Letters, 1990
- An experimental method for directly determining the interconnectivity of melt in a partially molten systemGeophysical Research Letters, 1988
- Melt migration beneath mid‐ocean spreading centersGeophysical Research Letters, 1987
- Detailed geological mapping by submersible of the East Pacific Rise axial graben near 13°NEarth and Planetary Science Letters, 1986
- The PT phase relations of a primary oceanite from the Reykjanes peninsula, IcelandLithos, 1980
- Periodicities in volcanism and longitudinal magma flow on the East Pacific Rise at 23°NGeophysical Research Letters, 1979
- Evidence for variability of magmatic processes and upper mantle heterogeneity in the axial region of the Mid-Atlantic Ridge near 22° and 36° NTectonophysics, 1979