Focused mantle upwelling beneath mid-ocean ridges: evidence from seamount formation and isostatic compensation of topography
- 1 September 1992
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 113 (1-2) , 41-55
- https://doi.org/10.1016/0012-821x(92)90210-m
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Solution-precipitation enhanced diffusional creep of partially molten olivine-basalt aggregates during hot-pressingPublished by Elsevier ,2003
- Simple 2-D models for melt extraction at mid-ocean ridges and island arcsPublished by Elsevier ,2002
- The East Pacific Rise and its flanks 8?18 N: History of segmentation, propagation and spreading direction based on SeaMARC II and Sea Beam studiesMarine Geophysical Research, 1992
- Hundreds of small volcanoes on the median valley floor of the Mid-Atlantic Ridge at 24–30° NNature, 1990
- Melt migration in a silicate liquid‐olivine system: An experimental test of compaction theoryGeophysical Research Letters, 1990
- Geochemical and structural studies of the Lamont seamounts: seamounts as indicators of mantle processesEarth and Planetary Science Letters, 1988
- Melt migration beneath mid‐ocean spreading centersGeophysical Research Letters, 1987
- On the cause of the asymmetric distribution of seamounts about the Juan de Fuca ridge: ridge-crest migration over a heterogeneous asthenosphereEarth and Planetary Science Letters, 1986
- A rolling mill effect in asthenosphere beneath oceanic spreading centersEarth and Planetary Science Letters, 1984
- Compositional and density stratification in oceanic lithosphere-causes and consequencesJournal of the Geological Society, 1977