Physics
Scientific paper
Dec 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993georl..20.2595l&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 20, no. 23, p. 2595-2598
Physics
15
Convective Heat Transfer, Earth (Planet), Lithosphere, Rheology, Stresses, Structural Basins, Temperature Dependence, Viscosity, Surface Layers, Two Dimensional Models, Variations
Scientific paper
Convection studies of temperature-dependent Newtonian and non-Newtonian rheology in aspect-ratio seven boxes have been carried out for volume averaged Rayleigh numbers between O(10(exp 5)) and O(10(exp 7)) Large lateral viscosity variations, O(10(exp 4)) are found for non-Newtonian cases with total temperature-dependent viscosity variations up to 250. Flow structures for both rheologies are distinguished by large-scale circulations with relatively stable descending limbs. Much larger hot thermal anomalies are found near the surface for non-Newtonian rheology. Lithospheric thinning is facilitated by non-Newtonian rheology because of stress-softening and the lubrication of the descending limbs by hot diapirs.
Larsen Tine B.
Malevsky Andrei V.
Smedsmo Jamie L.
Yuen David A.
No associations
LandOfFree
Temperature-dependent Newtonian and non-Newtonian convection: Implications for lithospheric processes does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Temperature-dependent Newtonian and non-Newtonian convection: Implications for lithospheric processes, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Temperature-dependent Newtonian and non-Newtonian convection: Implications for lithospheric processes will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-786362