Relative plate motion can not demonstrate the motion velocity of individual plate, while absolute plate motion can show the motion velocity in the stationary geospace.

The absolute plate motion model can be achieved by inverting the data set of the propagation rates and/or trends of volcanic chains to determine the origin in the angular space for the relative plate motion.

No direct relationship has been demonstrated between the direction of relative plate motion and linear indicators of movement direction on shallowly dipping foliations, thrusts and faults.

In this paper authors narrated paleomagnetism method of relative and absolute motion of terrane and at the same time indicated their inadequacy.

So the authors consider that the formation and evolution of the Chinese inland basins are the necessary result of plate movements since Paleozoic.

For this information, it can be induced that the rotative velocity of the liguid outer core presents similar nonuniformity, and the nonuniform rotation will have an effect on crust plate movement.

In order to surmount many deficiencies in determining the parameters of plate movement by least square(LS) method,we have set up a semiparametric model based on compensated LS principle.