Crustal accretion and dynamic feedback on mantle melting of a ridge centred plume: The Iceland case
Authors:
- Harro SchmelingHSHarro Schmeling
- Gabriele MarquartGMGabriele Marquart
- 1 February 2008
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 447 (1-4) , 31-52
Abstract
No abstract availableThis publication has 48 references indexed in Scilit:
- Numerical modelling of dyke interaction and its influence on oceanic crust formationTectonophysics, 2008
- Crust–mantle transition and Moho model for Iceland and surroundings from seismic, topography, and gravity dataTectonophysics, 2005
- Thermal models of oceanic crustal accretion: Linking geophysical, geological and petrological observationsGeochemistry, Geophysics, Geosystems, 2004
- Imaging the mantle beneath Iceland using integrated seismological techniquesJournal of Geophysical Research, 2002
- Mantle flow, melting, and dehydration of the Iceland mantle plumeEarth and Planetary Science Letters, 1999
- Dynamics of mantle flow and melting at a ridge-centered hotspot: Iceland and the Mid-Atlantic RidgeEarth and Planetary Science Letters, 1996
- Variable viscosity convection and partial melting in the continental asthenosphereJournal of Geophysical Research, 1996
- Crustal accretion model for Iceland predicts ‘cold’ crustGeophysical Research Letters, 1995
- Cold crust in a hot spotGeophysical Research Letters, 1994
- Heat flow and geothermal processes in IcelandTectonophysics, 1993