Based on the discussion of the dynamic process and thermodynamic effect of the Ordos Basin, as represented by the Zijinshan complex, the magma activity in the eastern part of the Ordos Basin with the respect of deep geological background, petrology, geochemistry, isotopic dating and tectonic evolution is studied. The research holds the view that the thermodynamic process is weakness and difficulty in the light of study on tectonic kinetics of basins. The thermodynamic process of the basin is evidently inhomogenous and the characteristics of the thermal basin are complicated and diverse.