摘要
Anhua-XupufaultbeltplaysaveryimportantroleintheformationofXuefengMountains.Thefaultbeltshowsanarc-structureextrudingtowardsNW.Faultrocks,microstructuresandhomogeneoustemperature(concentratedaround160°C)offluidinclusionsinthequartzveinsshowsthatthefaultbeltmainlyunderwentshallowbrittledeformationandthehighest-gradedynamicmetamorphicrockismylonitizedsericitephyllite.TheESR(ElectronSpinResonance)datingfromthequartzveinsinthefaultrocksshowsthatthefaultbeltunderwenttwointensefluidmovementstagesatYanshanian(156.9～136.2Ma,119.8～90.6Ma);moreovernotonlytheoccurrenceandmicrostructuresbutalsothehomogeneoustemperatureofthequartzveinsdevelopedinthattwostagesshowobviousdiversity,whichcanprovethatthereexiststhereversionperiodofMesozoicextensionandcompressionmovementofXuefengmountainsbetweenthesetwostages.
出版日期
2005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）
