The stability of the magma chamber is controlled by interior factors such as the behavior of activities and the cooling rate of the magma chamber as well as exterior factors like the extrusion and vibration of the rocks around the magma chamber. Under certain conditions, the activities of the rocks around the magma chamber can play a crucial role in the stability of magma chamber, especially in the area with frequent crustal movement. The aim of this study is to simulate the processes of the magma chambers of Laoheishan volcano in Wudalianchi area. On the basis of the heat conduction equation and the coupling of Duffing equations of the magma chamber, it is concluded that whether the Laoheishan magma chamber has been cooled or not is closely related to the heating history of the rocks around the magma chamber, and that the magma has approached complete solidification and some nonlinear processes must have existed in the dynamic system of the magma chamber.