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2011, 1. ed., ISBN 0521198003, vii, 232
"Mantle convection is the fundamental agent driving many of the geological features observed at the Earth's surface, including plate tectonics and plume volcanism... 
Heat | Plate tectonics | Plumes (Fluid dynamics) | Convection | Earth (Planet) Mantle | Earth Sciences | Earth | Mantle
Book
Journal of fluid mechanics, ISSN 0022-1120, 09/2015, Volume 778, pp. 721 - 764
We simulate numerically Boussinesq convection in non-rotating spherical shells for a fluid with a Prandtl number of unity and for Rayleigh numbers up to $10^{9... 
Papers | geophysical and geological flows | Bénard convection | boundary layers | NATURAL-CONVECTION | HEAT-TRANSFER | PHYSICS, FLUIDS & PLASMAS | NUSSELT NUMBER | SHEET-LIKE | MANTLE CONVECTION | Benard convection | VISCOUS BOUNDARY-LAYER | MECHANICS | MODELS | 3-DIMENSIONAL THERMAL-CONVECTION | ASPECT RATIO | ZONAL FLOW
Journal Article
Nature (London), ISSN 1476-4687, 2010, Volume 465, Issue 7298, pp. 602 - 605
Mobile belts are long-lived deformation zones composed of an ensemble of crustal fragments, distributed over hundreds of kilometres inside continental... 
TECTONICS | MULTIDISCIPLINARY SCIENCES | SUBDUCTION | SLAB | EAST | DYNAMIC TOPOGRAPHY | KINEMATICS | Earth | Tectonics (Geology) | Seismic tomography | Research | Mantle | Methods | Natural history | Geology | Plate tectonics | Lithosphere | Topography
Journal Article
Earth and Planetary Science Letters, ISSN 0012-821X, 1998, Volume 160, Issue 3, pp. 289 - 296
We consider a series of simple calculations with a step-function change in thickness of the lithosphere and imposed, far-field boundary conditions to... 
convection | mantle | mantle plumes | flood basalts | Flood basalt | Mantle | Lithosphere | Convection | Mantle convection | Mantle plume | GEOCHEMISTRY & GEOPHYSICS | BERMUDA
Journal Article
Journal of Geophysical Research: Solid Earth, ISSN 0148-0227, 09/2000, Volume 105, Issue B9, pp. 21795 - 21817
Small‐scale convection associated with instabilities at the bottom of the lithospheric plates on the Earth and other terrestrial planets occurs in the stagnant lid regime of temperature... 
SEISMIC ANISOTROPY | OCEANIC LITHOSPHERE | GEOCHEMISTRY & GEOPHYSICS | UPPER-MANTLE | CONTINENTAL LITHOSPHERE | INFINITE PRANDTL NUMBER | LEHMANN DISCONTINUITY | 3-DIMENSIONAL THERMAL-CONVECTION | HEAT-FLOW | VARIABLE-VISCOSITY FLUID | DYNAMIC RECRYSTALLIZATION
Journal Article
Journal Article
Geophysical journal international, ISSN 1365-246X, 2006, Volume 166, Issue 1, pp. 97 - 114
.... Convection is driven by a fixed temperature contrast between rigid boundaries. There are two distinct classes of solutions with strong and weak dipole contributions to the magnetic field, respectively. Non... 
convection | core flow | planetology | geomagnetic field | dynamo theory | inner core | Inner core | Core flow | Planetology | Convection | Dynamo theory | Geomagnetic field | GEODYNAMO MODELS | EARTHS CORE | GEOMAGNETIC-FIELD | INNER-CORE | GEOCHEMISTRY & GEOPHYSICS | SECULAR VARIATION | FLUID SHELLS | BOUNDARY HEAT-FLOW | COMPUTER-SIMULATION | CORE-MANTLE INTERACTIONS | NUMERICAL DYNAMOS | Magnetic fields | Earth Sciences | Sciences of the Universe | Geophysics | Applied geology
Journal Article