Relief evolution of the Continental Rift of Southeast Brazil revealed by in situ-produced <sup>10sup>Be concentrations in river-borne sediments
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The denudation dynamics of the Continental Rift of Southeast Brazil was studied.

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

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

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The results suggest a reduction in intraplate tectonic activity.

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