Erosion rates and mechanisms of knickzone retreat inferred from 10Be measured across strong climate gradients on the northern and central Andes Western Escarpment

Author:

Abbühl Luca M.1,Norton Kevin P.1,Jansen John D.2,Schlunegger Fritz1,Aldahan Ala,Possnert Göran3

Affiliation:

1. Institute of Geological Sciences; University of Bern; CH-3012; Bern; Switzerland

2. Department of Physical Geography and Quaternary Geology; Stockholm University; SE-106 91; Stockholm; Sweden

3. Tandem Laboratory; Uppsala University; SE-751 20; Uppsala; Sweden

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference62 articles.

1. El Niño forcing on 10Be-based surface denudation rates in the northwestern Peruvian Andes?;Abbühl;Geomorphology,2010

2. Agteca 2010 Global Historical Climatology Network (GHCN-Monthly database) Agteca.org http://www.agteca.org/climate.htm

3. Functional relationship between denudation, relief, and uplift in large mid-latitude drainage basins;Ahnert;American Journal of Science

4. A high-resolution 10Be profile from deep sea sediment covering the last 70 ka: indication for globally synchronized environmental events;Aldahan;Quaternary Science Reviews,1998

5. Estimating rates of denudation using cosmogenic isotope abundances in sediment;Bierman;Earth Surface Processes and Landforms,1996

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