The March 2, 2016 M 7.8 earthquake, 800 km off the west coast of southern Sumatra, Indonesia, occurred as the result of strike-slip faulting within the oceanic lithosphere of the Indo-Australia plate.
This event is located 600 km southwest of the major subduction zone that defines the plate boundary between the India/Australia and Sunda plates offshore Sumatra. At this location, the India/Australia plates move north-northeast relative to the Sunda plate at the velocity of about 55 mm/yr.
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