Publications des scientifiques de l'IRD

Cerpa N. G., Araya R., Gerbault Muriel, Hassani R. (2015). Relationship between slab dip and topography segmentation in an oblique subduction zone : insights from numerical modeling. Geophysical Research Letters, 42 (14), p. 5786-5795. ISSN 0094-8276.

Titre du document
Relationship between slab dip and topography segmentation in an oblique subduction zone : insights from numerical modeling
Année de publication
2015
Type de document
Article référencé dans le Web of Science WOS:000359316100014
Auteurs
Cerpa N. G., Araya R., Gerbault Muriel, Hassani R.
Source
Geophysical Research Letters, 2015, 42 (14), p. 5786-5795 ISSN 0094-8276
Slab dip controls the state of stress in an overriding plate and affects mountain building. Analog and numerical models have shown variations in tectonic regime induced by slab folding over the 660 km depth discontinuity zone in orthogonal convergence. Here using a three-dimensional model of oblique subduction (30 degrees) and accounting for free top surfaces, we show how slab folding generates an along-strike slab dip segmentation, inducing variations in topography of the overriding plate. When the subducting plate begins to curve forward, the elevation height rises inland and varies along the trench from 5 km to 2 km. The Andes are a suitable natural zone to compare our results with because of its linear margin and well-constrained plates kinematics. Thus, we provide a new explanation to the general decrease in elevation from the central to southern Andes, which still remains to be combined with other 3-D mechanisms to explain the actual Andean topography.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Géologie et formations superficielles [064]
Description Géographique
AMERIQUE DU SUD ; CHILI ; PEROU ; ANDES
Localisation
Fonds IRD [F B010064922]
Identifiant IRD
fdi:010064922
Contact