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The largest slow-slip event ever recorded in New Zealand
The Kapiti event started in early 2013 and is still going on. It is New Zealand’s largest slow-slip event ever recorded, equivalent to a magnitude 7.1 earthquake. We have 12 years of records in this region, which show three Kapiti events, each occurring roughly every five years. So far, this current event has as much as 15cm of movement over an area approximately 100km by 200km. The previous event in 2008 was equivalent to a magnitude 7.0 earthquake, but the movement was more concentrated: 30cm of movement over a smaller area near Kapiti Island. The 2013 slow-slip event evolved over the course of the year, moving north-eastward towards the North Island, with movement diminishing in late 2013-early 2014.
The fault in the Eketahuna earthquake would most likely have ruptured in the near future, but the added stress may have caused it to rupture earlier.
Slow-slip events do not universally increase stress on surrounding faults, they also relieve stress in some areas, and therefore may postpone an earthquake in an area of decreased stress.
F-E Region: Bay of Bengal
Time: 2014-05-21 16:21:50.4 UTC
Magnitude: 5.5
Epicenter: 87.92°E 18.17°N
Depth: 10 km
Status: A - automatic
geofon.gfz-potsdam.de...
Public ID 2014p384573
Universal Time May 23 2014 at 7:00:34
NZ Standard Time Friday, May 23 2014 at 7:00:34 pm
Latitude, Longitude -45.61, 167.18
Focal Depth 81 km
Magnitude 5.1ML
Location 45 km west of Te Anau
www.geonet.org.nz...
F-E Region: Aegean Sea
Time: 2014-05-24 09:25:03.5 UTC
Magnitude: 6.4
Epicenter: 25.38°E 40.28°N
Depth: 10 km
Status: A - automatic