Publications des scientifiques de l'IRD

Carretier Sébastien, Regard V., Vassallo R., Martinod J., Christophoul F., Gayer E., Audin Laurence, Lagane Christelle. (2015). A note on Be-10-derived mean erosion rates in catchments with heterogeneous lithology : examples from the western Central Andes. Earth Surface Processes and Landforms, 40 (13), p. 1719-1729. ISSN 0197-9337.

Titre du document
A note on Be-10-derived mean erosion rates in catchments with heterogeneous lithology : examples from the western Central Andes
Année de publication
2015
Type de document
Article référencé dans le Web of Science WOS:000362684200002
Auteurs
Carretier Sébastien, Regard V., Vassallo R., Martinod J., Christophoul F., Gayer E., Audin Laurence, Lagane Christelle
Source
Earth Surface Processes and Landforms, 2015, 40 (13), p. 1719-1729 ISSN 0197-9337
Millennial catchment-mean erosion rates derived from terrestrial cosmogenic nuclides are generally based on the assumption that the lithologies of the parent rock each contain the same proportion of quartz. This is not always true for large catchments, in particular at the edge of mountainous plateaus where quartz-rich basement rocks may adjoin sedimentary or volcano-sedimentary rocks with low quartz content. The western Central Andes is an example of this type of situation. Different quartz contents may be taken into account by weighting the TCN production rates in the catchment. We recall the underlying theory and show that weighting the TCN production rate may also lead to bias in the case of a spatial correlation between erosion rate and lithology. We illustrate the difference between weighted and unweighted erosion rates for seven catchments (16 samples) in southern Peru and northern Chile and show variations up to a factor of 2 between both approaches. In this dataset, calculated erosion rates considering only granitoid outcrops are better correlated with catchment mean slopes than those obtained without taking into account the geological heterogeneity of the drained watershed. This dataset analysis demonstrates that weighting erosion rates by relative proportions of quartz is necessary to evaluate the uncertainties for calculated catchment-mean erosion rates and may reveal the correlation with geomorphic parameters.
Plan de classement
Géologie et formations superficielles [064]
Description Géographique
PEROU ; CHILIE ; ANDES
Localisation
Fonds IRD [F B010065382]
Identifiant IRD
fdi:010065382
Contact