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Study finds abrupt quake motion ends ruptures, improving hazard assessments.
Scientists have identified a "stopping phase" signal during large earthquakes, which occurs when a rupture ends abruptly rather than slowing down.
This reversal in ground motion helps researchers pinpoint where the strongest shaking happens, particularly at fault segment boundaries.
The findings improve hazard assessments for regions like California and New Zealand, aiding disaster preparedness.
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El estudio encuentra que el movimiento abrupto del terremoto termina con rupturas, mejorando las evaluaciones de peligro.