摘要
TheChangjiangRiverDeltaisadeltaoftremendousscalewhichisformedunderthecontroloftideandtidalcurrents.ThestudyontheroleoftideandtidalcurrentsintheprocessofformationanddevelopmentoftheChangjiangRiverDeltacanprovideatypicalexamplefortheocean-continentinteractionprocessintheeastareaofourcountry.ThetideandtidalcurrentsintheBohaiSea,YellowSeaandEastChinaSeaatthepost-glacialtransgressionmaximumaresimulated,thesedimenttransportfieldinthePaleo-ChangjiangRiverEstuary(PCRE)anditsperipheralareaatthattimeiscalculated,andtheseabederosion/accretionpatternisobtainedaccordingtothedivergenceofsedimenttransportrate.Theresultsshowthatadistinctivewavebellyofstandingtidalwaveexistedatthepost-glacialtransgressionmaximumandthewavebellylinesprotrudedseawardsfromthewavebellypointinthemouthofthePCRE.Underthewavebellycontroltidalcurrentsconvergetoordivergefromthewavebell
出版日期
1999年02月12日(中国期刊网平台首次上网日期,不代表论文的发表时间)