Erosion rates and mechanisms of knickzone retreat inferred from 10Be measured across strong climate gradients on the northern and central Andes Western Escarpment-Reference-Cited by-同舟云学术

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

Published:2011-05-24 Issue:11 Volume:36 Page:1464-1473
ISSN:0197-9337
Container-title:Earth Surface Processes and Landforms
language:en
Short-container-title:Earth Surf. Process. Landforms

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

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/esp.2164/fullpdf

Reference62 articles.

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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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