A self‐consistent model of melting, magma migration and buoyancy‐driven circulation beneath mid‐ocean ridges
- 10 March 1989
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 94 (B3), 2973-2988
- https://doi.org/10.1029/jb094ib03p02973
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Along-axis variations in seafloor spreading in the MARK areaNature, 1987
- Global correlations of ocean ridge basalt chemistry with axial depth and crustal thicknessJournal of Geophysical Research, 1987
- Multi-channel seismic imaging of a crustal magma chamber along the East Pacific RiseNature, 1987
- Rheology and structure of olivine‐basalt partial meltsJournal of Geophysical Research, 1986
- The existence of a thin low-viscosity layer beneath the lithosphereEarth and Planetary Science Letters, 1986
- A possible explanation of gravity anomalies over mid‐ocean ridgesJournal of Geophysical Research, 1986
- Solution-precipitation enhanced diffusional creep of partially molten olivine-basalt aggregates during hot-pressingTectonophysics, 1984
- The deep structure of ocean ridges in a convecting mantleEarth and Planetary Science Letters, 1983
- Role of multistage melting in the formation of oceanic crustGeology, 1980
- A geophysical, geochemical, petrological model of the sub-marine lithosphereTectonophysics, 1979