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Seismically observable popular features of adult stagnant-top convection on the bottom of one’s lithosphere: Some scaling relationship

Seismically observable popular features of adult stagnant-top convection on the bottom of one’s lithosphere: Some scaling relationship 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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