M 7.1 - 32 km SE of Lata, Solomon Islands
- 2013-02-08 15:26:38 (UTC)
- 10.928°S 166.018°E
- 21.0 km depth
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Estimated Fatalities Origin - Review Status
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- Magnitude
- 7.1 mww
- Depth
- 21.0 km
- Time
- 2013-02-08 15:26:38 UTC
Moment Tensor Fault Plane Solution Finite Fault Slip Distribution information not specified.Tsunami 
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View Nearby Seismicity - Time Range
± Three Weeks - Search Radius
250.0 km - Magnitude Range
≥ 4.0
Contributors US
USGS National Earthquake Information Center, PDE
Tectonic Summary
The February 8, 2013, M 7.1 earthquake in the Santa Cruz Islands occurred as a result of shallow strike-slip faulting within the oceanic lithosphere of the Pacific plate, above the subduction zone interface between the Australia and Pacific plates. Focal mechanism solutions indicate that rupture occurred on either a right-lateral west-striking fault or a left-lateral north-striking fault. Finite-fault modeling of globally recorded seismic data for this earthquake is not able to distinguish between these two possibilities. At the location of this earthquake, the Australia plate moves towards the east-northeast with respect to the Pacific plate at a velocity of about 94 mm/yr. This event can be considered an aftershock of the damaging M 8.0 Santa Cruz Islands earthquake that occurred 2 days previously, 50 km to the northeast.
The February 8th earthquake is located adjacent to a complex section of the Australia-Pacific plate boundary, where the Solomon Trench to the west is linked to the New Hebrides (Vanuatu) Trench to the south by a short segment of dominantly strike-slip plate motion. The February 8th earthquake is located at the northern end of the New Hebrides (Vanuatu) segment. To the north and west of this event, the plate boundary changes in character, is oriented more west-to-east, and connects the segment ruptured by this event with the continuation of the subduction zone along the Solomon Islands.
Though close to the subduction zone plate boundary in the region, the depth and focal mechanism solutions of this M 7.1 earthquake indicate intraplate faulting within the overlying Pacific plate, rather than deeper thrust faulting directly related to the subduction process. The event was likely driven by the stresses generated by the earlier M 8.0 mainshock, similar to the M 7.0 February 6th, 01:54 UTC aftershock, 60 km to the northwest.
Hayes 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)