Menurut USGS, Gempa kali ini masih merupakan gempa susulan atau gempa
terusan dari akibat gempa dec 2004 lalu.
Gempa kali ini akibat strike-slip fault. Dengan rupture 15 Km
sepanjang 80 Km, bandingkan dengan gempa dec 2004 yang rupture zonenya
sepanjang 1200 km dengan lebar 200 Km.

RDP



========================
This earthquake occurred near the western boundary of the aftershock
zone of the devastating December 26th, 2004 earthquake. The aftershock
zone of the December 26th earthquake continues to be active and forms
a crescent-shaped region extending about 1200 km north of Sumatra,
Indonesia. The recent event was a strike-slip earthquake in the Burma
plate near its boundary with the India plate. Strike-slip earthquakes
generate horizontal motion across a fault. This is unlike the motion
caused by the December 26th earthquake that was the result of
thrust-faulting on the interface of the India plate and the Burma
plate, in which the India plate thrust beneath the overriding Burma
plate. Given the different mechanisms, the recent event did not occur
on the same fault that caused the Great Sumatra-Andaman Islands
earthquake. However, the two earthquakes are almost certainly related.
A great earthquake can trigger earthquake activity on faults that are
distinct from the main-shock fault plane, and separated from it by
tens or even hundreds of kilometers. A magnitude 7.2 earthquake is
considered a major earthquake, however the size of this recent
earthquake pales in comparison to the December 26th earthquake. A 7.2
strike-slip earthquake typically ruptures a 15 km by 80 km patch along
a fault, whereas the December, 2004 earthquake ruptured a patch of
fault about 1200 km long and 200 km wide.

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