This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1002/2015JB012721. This is version 1 of this Preprint.
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Seismic slip extends from maximum expected depth through the crust in 45-75 Ma oceanic lithosphere in the Indo-Australian intraplate region off the Sumatra-Andaman trench. Large (magnitude greater than 7) strike-slip earthquakes in this region can rupture multiple differently oriented faults. Rupture directivity modeling provides tentative support for active east-west oriented faults.
Earth Sciences, Geophysics and Seismology, Physical Sciences and Mathematics
Earthquake source observations, earthquake, body waves, Transform faults, oceanic crust, Sumatra, Finite-fault, Oceanic transform and fracture zone processes, Wharton Basin
Published: 2017-11-05 18:42
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