Bend Faulting at the Edge of a Flat Slab: The 2017 Mw7.1 Puebla‐Morelos, Mexico Earthquake

Bend Faulting at the Edge of a Flat Slab: The 2017 Mw7.1 Puebla‐Morelos, Mexico Earthquake

Abstract We present results of a slip model from joint inversion of strong motion and static Global Positioning System data for the Mw7.1 Puebla‐Morelos earthquake. We find that the earthquake nucleates at the bottom of the oceanic crust or within the oceanic mantle with most of the moment release o...

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Bibliographic Details
Main Authors: Diego Melgar, Xyoli Pérez‐Campos, Leonardo Ramirez‐Guzman, Zack Spica, Victor Hugo Espíndola, William C. Hammond, Enrique Cabral‐Cano
Format: Article
Language:English
Published: Wiley 2018-03-01
Series:Geophysical Research Letters
Subjects:
Subduction zones
Earthquake source observations
Intraplate earthquakes
Inverse theory
Geodesy
Ground motion
Online Access:https://doi.org/10.1002/2017GL076895
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https://doi.org/10.1002/2017GL076895

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