Measuring middle Pleistocene erosion rates with cosmic-ray-produced nuclides in buried alluvial sediment, Fisher Valley, southeastern Utah
Cosmic‐ray‐produced 10Be and 26Al in riverborne quartz sediment are commonly used to estimate average catchment‐scale erosion rates. Likewise, the concentrations of these nuclides in ancient sediments, stored in a depositional basin, carry a record of past erosion rates in the sediment source area....
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Veröffentlicht in: | Earth surface processes and landforms 2005-08, Vol.30 (8), p.1051-1067 |
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