\nThe January 27, 2006, M 7.6 Banda Sea earthquake occurred as the result of deep oblique normal faulting approximately 397 km beneath the Banda Sea, in the tectonically complex region of southeastern Indonesia. Here, the overall convergence between the Australia and Sunda plates is accommodated by the relative motions of numerous small microplates, including the Banda Sea and Timor microplates local to this event. Focal mechanism solutions for the earthquake indicate that rupture occurred on either a northeast or south-southeast-striking, moderately dipping normal fault. Slip on a fault of either orientation would accommodate the down-dip extension of the Australia slab that is implied by the normal-component of the faulting solution. At the location of the event, the Australia plate moves northward relative to the Sunda plate at a velocity of about 70 mm/yr. The earthquake occurred in the inclined seismic zone that dips northward from the Timor trough and that marks the position of the subducted Australia plate at depth. \n
\n\nUntil recently in geologic time, the Australia plate subducted beneath the Timor microplate at the Timor trough. Within geologically recent time, northward subduction of Australia beneath the Timor plate has largely ceased, and the northward motion of the Australia plate relative to the Sunda plate is now accommodated substantially by the southward subduction of the Banda Sea microplate beneath the Timor microplate on the northern boundary of the Timor microplate. The subducted Australia plate nonetheless remains intensely seismic, probably because of high stresses that are generated by the distortion of the slab at depth. \n
\n\nThe tectonically complex region surrounding the Banda Sea experiences large earthquakes fairly regularly. Eight other M 7 or larger earthquakes have occurred within 400 km of the January 27th event over the preceding 40 years. The largest was a M 7.3 earthquake in December 1992, nearly 200 km to the southeast, with no associated damage or casualties.\n
\n\nEarthquakes that have focal depths greater than 300 km are commonly termed “deep-focus” earthquakes. Deep-focus earthquakes cause less damage on the ground surface above their foci than similar-magnitude shallow-focus earthquakes, but large deep-focus earthquakes may be felt at great distance from their epicenters. The largest recorded deep-focus earthquake prior to this January 2006 earthquake was a M 8.2 event that occurred at a depth of 630 km within the subducted Nazca plate beneath South America near the northern Bolivian border in 1994. A larger event has since occurred—namely the M 8.3 earthquake that occurred at a depth of 600 km within the subducted Pacific plate beneath the Sea of Okhotsk offshore of northeastern Russia in 2013. The M 8.3 Sea of Okhotsk earthquake was felt all over Asia, as far away as Moscow, and across the Pacific Ocean along the western seaboard of the United States (though at distant locations, individuals reporting having felt the event were likely very favorably situated for the perception of small ground motions). The M 8.2 Bolivian deep-focus earthquake in 1994 had similarly been reported by individuals in North America at great distance from the epicenter.\n
\n\nOver the past century, 74 earthquakes with a magnitude of M 7+ have occurred at depths greater than 300 km globally; 7 of these were located in the same region as the January 27, 2006, event. The largest nearby event at these depths was a M 7.9 earthquake in June 1996, several hundred kilometers to the southwest and 210 km deeper than the January 27th event. The June 1996 event resulted in only minor damage at Kupang, Indonesia.\n
\n\nHayes et al. (2016) Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015, USGS Open-File Report 2016-1192. (5.2 MB PDF)\n
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