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- W2365713168 abstract "The constraint of ductile shear deformation on petro-chemical behavior has always been a focus for geologists.The Guachehe town area in Tongcheng of Anhui is a meeting place of the eastern fringe of the Dabie orogen and the Tan-Lu Fault zone,where the two tectonic systems are both developed in terms of ductile shear zone,providing conditions for making comparative analysis.Different tectonic systems and different phases of felsic ductile shear zones show similar regularity for volume change and element migration in the process of mylonitization,the volume loss and element migration become even more remarkable as deformation increases,the loss can be up to 32.18% and the migration is shown as move-out of SiO2,K2O and Na2O,and move-in of Fe2O3,CaO and MgO.Compared with felsic shear zone,mafic brittle-ductile shear zone shows a reverse law during mylonitization,i.e.,volume increase of 21.63%-186.60% and considerable move-in of SiO2 and move-out of Fe2O3 and CaO." @default.
- W2365713168 created "2016-06-24" @default.
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- W2365713168 date "2012-01-01" @default.
- W2365713168 modified "2023-09-25" @default.
- W2365713168 title "Element and mass balance analysis of ductile shear zone in the Guachehe town area,Tongcheng,Anhui" @default.
- W2365713168 hasPublicationYear "2012" @default.
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