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Relief evolution of the Continental Rift of Southeast Brazil revealed by in situ-produced 10Be concentrations in river-borne sediments
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文摘

The denudation dynamics of the Continental Rift of Southeast Brazil was studied.

The seaward-facing scarps are more denudated than the inland-facing scarps.

Lithology, climate, catchment relief and gradient, determine the denudation rates.

The results suggest a reduction in intraplate tectonic activity.

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