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Is the Aftershock Zone Area a Good Proxy for the Mainshock Rupture Area?
[post]
2020
unpublished
Large earthquakes are usually followed by sequences of small earthquakes, exhibiting a mainshock-aftershock pattern. The locations of aftershocks are often observed to be on the same fault plane as the mainshock and used as proxies for its rupture area. However, there has been limited research on how well aftershock location actually approximates mainshock rupture area. Furthermore, recent developments in earthquake relocation techniques have led to great improvements in the accuracy of
doi:10.31223/osf.io/cp9vn
fatcat:gdfihhs2frdltl3sb2zdqj5tiu