Three‐dimensional flow and temperature perturbations due to a transform offset: Effects on oceanic crustal and upper mantle structure
Open Access
- 10 April 1988
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 93 (B4) , 2955-2966
- https://doi.org/10.1029/jb093ib04p02955
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- A tectonic model for ridge-transform-ridge plate boundaries: Implications for the structure of oceanic lithospherePublished by Elsevier ,2003
- Streamline upwind/Petrov-Galerkin formulations for convection dominated flows with particular emphasis on the incompressible Navier-Stokes equationsPublished by Elsevier ,2003
- Magma migration beneath an ocean ridgePublished by Elsevier ,2002
- The spacing of rift axis highs: dependence upon diapiric processes in the underlying asthenosphere?Published by Elsevier ,2002
- Three-dimensional temperature structure of a ridge-transform-ridge systemPublished by Elsevier ,2002
- Segmentation of mid-ocean ridgesNature, 1985
- The Generation and Compaction of Partially Molten RockJournal of Petrology, 1984
- Petrogenesis of Basalt Glasses from the Tamayo Region, East Pacific RiseJournal of Petrology, 1984
- A rolling mill effect in asthenosphere beneath oceanic spreading centersEarth and Planetary Science Letters, 1984
- A critical evaluation of upstream differencing applied to problems involving fluid flowComputer Methods in Applied Mechanics and Engineering, 1976