Erosion rates of the Bhutanese Himalaya determined using in situ-produced 10Be

Western Bhutan provides an ideal setting to understand the interplay between uplift, erosion, and fluvial sediment transport in an active mountain environment. Using in situ-produced 10Be (49 samples) and 26Al (5 samples) in fluvial sediment from nested catchments throughout the Puna Tsang Chhu drai...

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Veröffentlicht in:	Geomorphology (Amsterdam, Netherlands) Netherlands), 2015-03, Vol.233, p.112-126
Hauptverfasser:	Portenga, Eric W., Bierman, Paul R., Duncan, Chris, Corbett, Lee B., Kehrwald, Natalie M., Rood, Dylan H.
Format:	Artikel
Sprache:	eng
Schlagworte:	Beryllium Bhutan Cosmogenic nuclide Denudation Drainage basins Erosion Erosion rate Geomorphology Himalayas Mathematical analysis Minerals Mountain environments Sediment Sediment transport Uplift
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