The elastic fields induced by non-elastic shear deformations with an elliptic inhomongeneity embedded in the transversely isotropic matrix were presented.

Constraints of ductile shear deformation on rock geochemical behavior-an example from the Bashikaogong ductile shear zone in the northern Altyn Tagh;

The characteristics of the ductile shear deformation developed between the Neoarchaeozoic Se erdengshan Group,and Neoarchaeozoic to Paleoprozoic gneissic tonalite (the basement),and the Dulahala and Jianshan formations of the Baiyun ebo Group ,and the Shujigou and Zenglongchang formations of the Zha ertaishan Group, Changcheng System (the cover)are identical.