NW-trending ductile shearing process i n Taishan area took place at the end of archaean, belonged to moderate-high temperature shearing deformation.

• 泰山地区北西向韧性剪切作用发生在构造体制从韧塑性变形向脆性变形转化的太古宙末期，属于中高温变形环境条件下的剪切变形。