Regolith evolution on the millennial timescale from combined U-Th-Ra isotopes and in situ cosmogenic 10Be analysis in a weathering profile (Strengbach catchment, France)
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文摘

Analysis of U-series isotopes and in situ 10Be in a single regolith profile.

Independent determination of long term regolith denudation and production rates.

Lower regolith is the most suitable place to quantify regolith production rate.

A high spatial resolution profile is required for an extensive modeling of in situ 10Be.

Higher temporal variability of physical erosion than chemical weathering.

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