摘要
Therearetwogradesofnetwork-typetextureinmetamorphicperidotitefromtheKudaophiolite,Xinjiang,China,Thefirstgraduationconsistsofcoarse-grainedolivinewithplasticdeformationfabrics,orthopyroxeneandminorclinopyroxeneandCr-spinel.Thesecondgraduationconsistsofsmallmineralsfillingamongthemineralgrainsofthefirstgraduation.Fourkindsofassemblagescontainingtremolitehavebeendiscoveredinthesecondgraduation,whichwereformedduringmantlepartialmeltingandmantlemetasomatismofahighlydepletedperidotite.
出版日期
1997年04月14日(中国期刊网平台首次上网日期,不代表论文的发表时间)