Continuous swarm-like seismicity: the Wanganui, New Zealand, earthquakes
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/75/2/493/1654072/75-2-493.pdf
Reference50 articles.
1. The New Zealand seismograph network
2. Subcrustal earthquakes beneath New Zealand; Locations determined with a laterally inhomogeneous velocity model
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1. Crust and upper-mantle structure of Wanganui Basin and southern Hikurangi margin, North Island, New Zealand as revealed by active source seismic data;Geophysical Journal International;2017-07-20
2. Quantifying seismicity associated with slow slip events in the Hikurangi margin, New Zealand;New Zealand Journal of Geology and Geophysics;2016-01-02
3. Crustal Structure and Origin of Basins Formed Behind the Hikurangi Subduction Zone, New Zealand;Origin and Evolution of Sedimentary Basins and Their Energy and Mineral Resources;2013-03-18
4. Cumulative rate analysis (CURATE): A clustering algorithm for swarm dominated catalogs;Journal of Geophysical Research: Solid Earth;2013-02
5. Characterizing earthquake recurrence parameters for offshore faults in the low-strain, compressional Kapiti-Manawatu Fault System, New Zealand;Journal of Geophysical Research;2007-12-29
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