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The large regional earthquake (2008 February 21, M = 6.0) with epicentre near Wells, Nevada, occurred within a few hundred kilometres of the High Lava Plains (HLP) seismic experiment stations when the network was near its full deployment (>100 stations with 10–30 km station spacing). The Wells earthquake provides an excellent opportunity to address two questions: What is the effect of small epicen...

High-resolution phase-velocity maps using data from an earthquake recorded at regional distances by a dense broad-band seismic network