Mantle convection and stability of depleted and undepleted continental lithosphere
- 10 February 1997
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 102 (B2) , 2771-2787
- https://doi.org/10.1029/96jb03271
Abstract
No abstract availableKeywords
This publication has 48 references indexed in Scilit:
- The experimental deformation of dunitePublished by Elsevier ,2003
- Glacial isostatic adjustment and Earth rotation: Refined constraints on the viscosity of the deepest mantleJournal of Geophysical Research, 1996
- Segregation of subducted oceanic crust in the convecting mantleJournal of Geophysical Research, 1994
- Onset of thermal convection in fluids with temperature‐dependent viscosity: Application to the oceanic mantleJournal of Geophysical Research, 1994
- Heat flow and heat generation in the Archaean Dharwar cratons and implications for the Southern Indian Shield geotherm and lithospheric thicknessTectonophysics, 1991
- The vertical distribution of radiogenic heat production in the Precambrian crust of Norway and Sweden: Geothermal implicationsGeophysical Research Letters, 1987
- Secondary convection and the growth of the oceanic lithospherePhysics of the Earth and Planetary Interiors, 1984
- Stability of the oceanic lithosphere with variable viscosity: an initial-value approachPhysics of the Earth and Planetary Interiors, 1984
- Rifting process and thermal evolution of the continental margin of Eastern Canada determined from subsidence curvesEarth and Planetary Science Letters, 1980
- The heat flow through oceanic and continental crust and the heat loss of the EarthReviews of Geophysics, 1980