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The structure of the crust and upper mantle to depths of 320 km beneath the Kaapvaal craton, from P wave arrivals generated by regional earthquakes and mining-induced tremors

GeophysicsKaapvaal CratonEngineeringStructural GeologySeismologySeismic WaveMining-induced TremorsGeologyLithosphereCrust-mantle InteractionRegional EarthquakesEarth ScienceCratonTectonics