Fractal and Self-Organization Developed in Ductile Deformation in the Crust of Southern Liaoning
辽南地壳韧性剪切变形中的分形及自组织

On the basis of the studies on the deformational features of the crust of Southern Liaoning,Fractal and self - organization phenomena developed in sheared folds, metamorphic segregational layers, S - C structures, nonsymmetric rotational porphyroclast and the grain size distribution of dynamic resrystallied quartz and its boundary have been studied detail. The fractal dimension of the grain size distribution and grain boundary of dynamic recrystallized quartz have been presented and also the genetic relationship between the metamorphic segregational layers and shear heating has been discussed.