Differences in 10Be concentrations between river sand, gravel and pebbles along the western side of the central Andes-Reference-Cited by-同舟云学术

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Differences in 10Be concentrations between river sand, gravel and pebbles along the western side of the central Andes

Published:2015-04 Issue: Volume:27 Page:33-51
ISSN:1871-1014
Container-title:Quaternary Geochronology
language:en
Short-container-title:Quaternary Geochronology

Author:

Carretier S.,Regard V.,Vassallo R.,Aguilar G.,Martinod J.,Riquelme R.,Christophoul F.,Charrier R.,Gayer E.,Farías M.,Audin L.,Lagane C.

Publisher

Elsevier BV

Subject

Earth and Planetary Sciences (miscellaneous),Stratigraphy,Geology

Reference94 articles.

1. Erosion rates and mechanisms of knickzone retreat inferred from 10Be measured across strong climate gradients on the northern and central Andes Western Escarpment;Abbuehl;Earth Surf. Proc. Land.,2011

2. Corrigendum: El Nino forcing on 10Be-based surface denudation rates in the northwestern Peruvian Andes? (vol. 123, pg 257, 2010);Abbuehl;Geomorphology,2011

3. Grain size-dependent 10Be concentrations in alluvial stream sediment of the Huasco Valley, a semi-arid Andes region;Aguilar;Quat. Geochronol.,2014

4. Variability in erosion rates related to the state of landscape transience in the semi-arid Chilean Andes;Aguilar;Earth Surf. Proc. Land,2011

5. Large rockslides in the Southern Central Andes of Chile (32–34.5 degrees S): tectonic control and significance for quaternary landscape evolution;Antinao;Geomorphology,2009

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