Post-rift influence of small-scale convection on the landscape evolution at divergent continental margins
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文摘
Small-scale convection produces intermittent vertical movement at continental margins. The movements are amplified with the presence of a less viscous lithospheric mantle. Great post-rift variability in the denudation rate induced by mantle convection. Small-scale convection can contribute to sustain a preexistent escarpment.

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