摘要
Consideringtheheterogeneityofgeomechanicalmaterials,seismicityduringbrittlerockfailureundercompressiveloadingonthesamplewithanoriginalweakzoneissimulatedbyusingrockfailureprocessanalysiscode(RFPA2D).Therun-throughprocessofweakzone,theformingofnewfaultandassociatedmicro-seismicitiesarestudied.Themodelingdemonstratesthetotalprocessofsourcedevelopmentofearthquakefromdeformation,micro-failuretocollapseandthebehavioroftemporal-spatialdistributionofmicro-seismicities.Thestress,strainandthetemporal-spatialdistributionofmicro-seismicitieslife-likelyportrayedthephenomenaoflocalizationandtemporal-spatialtransitions,whichissimilartothoseobservedinourrealcrust.Also,theresultsobtainedinsimulationsareinagreementwithorsimilartothereportedexperimentalobservations.
出版日期
2002年01月11日(中国期刊网平台首次上网日期,不代表论文的发表时间)