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The potential tectonic and climatic controls on erosion rates in the European Alps and other mountain belts remain strongly debated. We have quantified denudation rates at catchment scales using in situ produced cosmogenic nuclides ( 10 Be) in stream sediments, sampled at the outlets of twelve variously sized (27–1072km 2 ) catchments of the Ecrins–Pelvoux massif (French Western Alps),...
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