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Tens of thousands of earthquakes are catalogued by the New Zealand geohazards monitoring agency, GeoNet (Petersen et al. Citation2011), across the country every year (https://quakesearch.geonet.org.nz/). An earthquake’s nucleation location – either specified in two dimensions by latitude and longitude (epicentre) or additionally including depth information in the third dimension (hypocentre) – is a fundamental parameter in the catalogue.
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