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Modelling the evolution of propagation and runout from a gravel–silty clay landslide to a debris flow in Shaziba, southwestern Hubei Province, China

Geotechnical EngineeringEarth ScienceEngineeringGravel–silty Clay LandslideGeomorphologyRock SlopeDebris FlowGeographyGeomechanicsSouthwestern Hubei ProvinceLandslide RiskEarth FlowSediment TransportSocial SciencesRock Properties