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THE DUCTILE MOBILITY CHARACTERISTICS OF THE TAN-LU FAULT IN THE MIDDLE OF ANHUI

Xu Wei;Tong Jinsong(Anhui Academy of Geological Survey, Hefei 230001)  
It has been disclosed that the ductile mobility of the Tan - Lu Fault in the Fuchashan area of middle of Anhui is characterizedby its product of large - scaled ductile shear zones and the tectonites of variety of myonites. As a result, the metamorphosed and deformed geological bodies in the Fuchashan area is in a framework of lenticular horses confined by shear zones typical of left - handed strike - slipshearing that formed in the early to middle Jurassic.
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