Seismically observable top features of adult stagnant-lid convection on the bottom of one’s lithosphere: Certain scaling relationships

Seismically observable top features of adult stagnant-lid convection on the bottom of one’s lithosphere: Certain scaling relationships 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 […]

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