Publications des scientifiques de l'IRD

Audin Laurence, Benavente C., Alvarado A., Zerathe S., Yepes H., Champenois J., Baize S., Delgado F., Beauval Céline, Robert X. (2016). Neotectonic activity in Ecuador and Peru, from geomorphic to geodetic data, focus around Andean megacities. In : 7th International INQUA meeting on Paleoseismology, Active Tectonics and Archeoseismology (PATA). s.l. : INQUA, 4 p. PATA : International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology, 7.

Titre du document
Neotectonic activity in Ecuador and Peru, from geomorphic to geodetic data, focus around Andean megacities
Année de publication
2016
Type de document
Colloque
Auteurs
Audin Laurence, Benavente C., Alvarado A., Zerathe S., Yepes H., Champenois J., Baize S., Delgado F., Beauval Céline, Robert X.
In
7th International INQUA meeting on Paleoseismology, Active Tectonics and Archeoseismology (PATA)
Source
s.l. : INQUA, 2016, 4 p.
Colloque
PATA : International INQUA Meeting on Paleoseismology, Active Tectonics and Archeoseismology, 7.
The Andean range stretches for thousands of kilometers from Patagonia to Venezuela and its recent tectonic evolution results from the ongoing subduction of the Nazca plate. Less studied than the subduction mega earthquakes, several M>7 continental earthquakes did affect the Andean human settlements since the Pre Incaic period. Although neglected in terms of archaeoseismic or neotectonic studies, the impacted regions display exponentially growing megacities, highly exposed to seismic hazards. In this study, we focus on investigating crustal deformation along newly described fault systems, in a seismically active urban setting (in Peru and Ecuador). High resolution satellite images, geodetic data, georadar and field studies provide striking examples and evidences of the ongoing tectonic deformation that can be the longer-term Quaternary geomorphic record. We focus here on the Quito and Ibarra regions in northern Ecuador, and on Arequipa and Cuzco regions in southern Peru.
Plan de classement
Géologie et formations superficielles [064] ; Géophysique interne [066] ; Télédétection [126]
Localisation
Fonds IRD [F B010067221]
Identifiant IRD
fdi:010067221
Contact