August 12, 2016 Earthquake: Loyalty Islands, New Caledonia

Felt at Namosi, Fiji and at Noumea, New Caledonia. Noumea, Sud, New Caledonia - CDI: 6; Namosi, Central, Fiji Islands - CDI: 2

Tectonic Summary

The August 12, 2016 M 7.2 earthquake east of New Caledonia in the southwest Pacific, and the North Fiji Basin, occurred as the result of shallow strike-slip faulting on or near the plate boundary between the Australia and Pacific plates. At the location of this earthquake the regional plate boundary is in a zone of transition, moving from east-northeastward-oriented subduction of Australia beneath Pacific at the New Hebrides Trench to the west, to southwest-northeast oriented left-lateral transform faulting between the two plates just south of this earthquake. The location of the August 12 event also lies just south and west of the Central Spreading Ridge, a zone of back-arc spreading accommodating some of the divergence between the New Hebrides and Tonga subduction zones. The focal mechanism solution of the August 12 event implies faulting occurred as the result of either right-lateral slip on a fault oriented east-southeast, or left-lateral slip oriented south-southwest. Such a mechanism is inconsistent with the major Australia-Pacific plate boundary, and may instead indicate association with local back-arc spreading. At the location of this earthquake, the Australia plate moves towards the east-northeast with respect to the Pacific at a rate of approximately 75 mm/yr. Spreading rates along the Central Spreading Ridge are also around 75-80 mm/yr.

While commonly plotted as points on maps, earthquakes of this size are more appropriately described as slip over a larger fault area. Strike-slip events of the size of the August 12, 2016 earthquake are typically about 80x15 km in size (length x width). The New Hebrides (Vanuatu) Arc and the North Fiji Basin are very active seismically. Over the preceding century, the region within 250 km has hosted seven other M 7 or larger events, and two-dozen or more earthquakes of M 6.5 or larger. The largest of these was a M 7.6 left-lateral strike slip event on the Australia-Pacific plate boundary in March 1990, 215 km to the east of the August 12 earthquake. A M 7.5 event 230 km to the west in January 1998 also occurred as the result of left-lateral strike-slip faulting. Over the two hours following the August 12, 2016 earthquake, 6 aftershocks of M 4.5-5.4 had occurred, roughly aligned in a west-northwest - south-southeast orientation; similar to the right-lateral plane of the focal mechanism solution.

(above from reference #13456)