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Sliding within grains and between grains, dislocation structures and partial recovery are deformation micromechanisms of the mylonites in Changle-Nan' ao ductile shear zone. Our researches show that the mylonites formed in greenschist facies (300--350 o C, 15km) and occured during the processes of recovery and recrystallization. Differential palaeostress and strain rates calculated by dislocation...
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