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