Abstract
High quality GPS and differential InSAR data have been collected for determining the ground deformation associated with the September 2010 Darfield (Canterbury) earthquake. We report preliminary results from a subset of these data and derive a preliminary source model for the earthquake. While the majority of moment release in the earthquake occurred on the strike-slip Greendale Fault a number of other fault segments were active during the earthquake including a steeply southeast-dipping thrust fault coincident with the earthquake hypocentre.
Cite
CITATION STYLE
Beavan, J., Samsonov, S., Motagh, M., Wallace, L., Ellis, S., & Palmer, N. (2010). The darfield (canterbury) earthquake: Geodetic observations and preliminary source model. Bulletin of the New Zealand Society for Earthquake Engineering, 43(4), 228–235. https://doi.org/10.5459/bnzsee.43.4.228-235
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.