Seismically observable popular features of adult stagnant-top convection at the base of your own lithosphere: Specific scaling matchmaking

adminsalir-en-tus-30 visitorsLeave a Comment

Small-scale convection transfers heat from the asthenosphere into the base of the lithosphere. Scaling constraints are obtained on features associated with such convection that may be resolved by seismic studiespact notation arises by simply representing rheology: viscosity changes by a factor of e with a temperature increase of T? and the minimum viscosity in the asthenosphere is ?0. The geothermal … Read More