Premium
Revisiting the Canterbury earthquake sequence after the 14 February 2016 M w 5.7 event
Author(s) -
Herman Matthew W.,
Furlong Kevin P.
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2016gl069528
Subject(s) - aftershock , seismology , geology , induced seismicity , intraplate earthquake , foreshock , seismic hazard , magnitude (astronomy) , sequence (biology) , submarine pipeline , tectonics , oceanography , physics , genetics , astronomy , biology
On 14 February 2016, an M w 5.7 (GNS Science moment magnitude) earthquake ruptured offshore east of Christchurch, New Zealand. This earthquake occurred in an area that had previously experienced significant seismicity from 2010 to 2012 during the Canterbury earthquake sequence, starting with the 2010 M w 7.0 Darfield earthquake and including four M w ~6.0 earthquakes near Christchurch. We determine source parameters for the February 2016 event and its aftershocks, relocate the recent events along with the Canterbury earthquakes, and compute Coulomb stress changes resolved onto the recent events and throughout the greater Christchurch region. Because the February 2016 earthquake occurred close to previous seismicity, the Coulomb stress changes resolved onto its nodal planes are uncertain. However, in the greater Christchurch region, there are areas that remain positively loaded, including beneath the city of Christchurch. The recent earthquake and regional stress changes suggest that faults in these regions may pose a continuing seismic hazard.