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Seismic evidence for repeated vertical fluid flow through polygonally faulted strata in the Canterbury Basin, New Zealand

Fault GeometryMarine GeologyEarthquake EngineeringEngineeringSeismic CycleStructural GeologySeismologyEarthquake SourceCivil EngineeringNew ZealandGeomechanicsGeologyEarthquake RuptureCanterbury BasinEngineering GeologySeismic EvidenceEarth ScienceTectonics