May 2018 (v1)
Publication
International audience
Uploaded on: December 4, 2022
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May 2018 (v1)Publication
International audience
Uploaded on: December 4, 2022 -
January 2021 (v1)Journal article
Megathrust ruptures and the ensuing postseismic deformation cause stress changes that may induce seismicity on upper plate crustal faults far from the coseismic rupture area. In this study, we analyze seismic swarms that occurred in the north Ecuador area of Esmeraldas, beginning two months after the 2016 Mw7.8 Pedernales, Ecuador megathrust...
Uploaded on: December 4, 2022 -
March 6, 2019 (v1)Journal article
The April 2016 Pedernales earthquake ruptured a 100 km by 40 km segment of the subduction zone along the coast of Ecuador in an Mw 7.8 megathrust event east of the intersection of the Carnegie ridge with the trench. This portion of the subduction zone has ruptured on decadal time scales in similar size and larger earthquakes, and exhibits a...
Uploaded on: December 4, 2022 -
February 2020 (v1)Journal article
International audience
Uploaded on: December 4, 2022