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ID:39910848
大小:5.30 MB
页数:44页
时间:2019-07-14
《Cordier_dislocation and slip system of mantle minerals》由会员上传分享,免费在线阅读,更多相关内容在学术论文-天天文库。
1、6DislocationsandSlipSystemsofMantleMineralsPatrickCordierLaboratoiredeStructureetPropriétésdel'EtatSolide(ESACNRS8008)UniversitédesSciencesetTechnologiesdeLille59655Villeneuved'Ascq-Cedex,FranceINTRODUCTIONThischapterfocusesondislocationsandslipsystemsthata
2、reresponsiblefortheplasticflowofhigh-pressuremantleminerals.Afterbrieflyintroducingsomebasicconceptsoncrystalplasticity,wedescribesomerecentexperimentaladvancesofthelastdecadethathavecontributedtoourunderstandingoftherheologyofmantleminerals.Amongthem,wedes
3、cribesomeprogressintheachievementofdeformationexperimentsunderhighpressure.AmoredetailedreviewispresentedbyDurhametal.(thisvolume).WepresentthenanovelTransmissionElectronMicroscopy(TEM)technique:LargeAngleConvergentBeamElectronDiffraction(LACBED),whichisver
4、ywelladaptedtothecharacterizationofdislocationsinbeamsensitivematerials,aswellasthedeterminationofdislocationBurgersvectorsandcharactersfromthefineanalysisofX-raydiffractionpeakbroadening.Thepresentreviewisinthecontinuityofthepaperentitled“PlasticRheologyof
5、Crystals”byPoirier,publishedin1995in“MineralPhysics&Crystallography—AHandbookofPhysicalConstants”(AGUReferenceShelf2).Poirier'spaperreviewedtheplasticityofsomeimportantmineralsincludingolivineandpyroxenes.Concerningthesetwominerals,thereaderisinvitedtorefer
6、toPoirier'scontribution.In1995,Poirierstatedabouthigh-pressuremantleminerals:“Despitetheirimportancefortherheologyofthetransitionzoneandthelowermantle,thereisnoinformationontheplasticityofthehigh-pressuremantlemineralsintherelevantconditionsoftemperatureand
7、pressure.”Sevenyearslater,thesituationhassignificantlyevolvedandisstillrapidlychanging.Itistheaimofthispapertohighlighttheserecentadvances.BASICCONSIDERATIONSPlasticflowisbasicallyatransportphenomenoncontrolledbythemotionofdefects:pointdefects,dislocations,
8、orgrainboundaries.Thedrivingforceisprovidedbytheappliedshearstress.Inmanycases,deformationisproducedbythemotionofdislocationsandthepresentpaperwillfocusonthisaspectonly.ThestrainratethenobeystheOrowan'
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