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Publikováno v:
Geophysical Research Letters
Alluvial rivers aggrade, incise, and adjust their sediment-transport rates in response to changing sediment and water supply. Fluvial landforms, such as river terraces, and downstream stratigraphic archives may therefore record information about past
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1cdca4024c1481d3649bd55d73821f46
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015419
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5015419
