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• Defined a ring-shaped region with the velocity of zero named Quasi-static Region.
• Quasi-static Region is the boundary of collapse during impact.
• Quasi-static Region has stable propagation characteristics.
• Changes in particle rheological properties occur at Quasi-static Region.
In this paper, through experiments and DEM simulations, it is found that there is a ring-shaped region named Quasi-static Region between the particles expanding outward and the particles collapsing inward during the impact process. Quasi-static Region is always generated from the impact point at the same time, and then spreads out at a uniform speed. During the propagation of Quasi-static Region, the velocity of the particles in the particle extend region varies linearly in space and time. And the change rate is only related to the properties of the particle system. The simulation results show that the particle flow in Quasi-static Region is elastic-inertial flow, while the particle flow expanding outward and collapsing inward is inertial flow.