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Abstract Characterizing the inelastic strain field around co-seismic faults is a key to understanding earthquake rupture processes. We aim to detect zones of inelastic deformation around surface ruptures, using Anisotropy… Click to show full abstract
Abstract Characterizing the inelastic strain field around co-seismic faults is a key to understanding earthquake rupture processes. We aim to detect zones of inelastic deformation around surface ruptures, using Anisotropy of Magnetic Susceptibility (AMS) analyses. To characterize the paleo-seismic setting we measured 29 normal faults, which cut the late Pleistocene lacustrine Lisan Formation and were associated with shallow (
Keywords:
zones inelastic;
deformation around;
inelastic deformation;
surface ruptures;
around surface
Journal Title: Tectonophysics
Year Published: 2020
Link to full text (if available)
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Journal Title: Tectonophysics
Year Published: 2020
Link to full text (if available)
Share on Social Media: Sign Up to like & get
recommendations!