When the impact pressure was lower than 6395GPa the macroscopic cracks in the crater area were mainly distributed on the side of the crater while the impact pressure exceeds 6395GPa and they were dist

This suggests that the location and distribution of cracks in the crater area are dependent on the impact pressure. Lower impact pressures result in cracks forming on the sides of the crater, while higher pressures result in cracks forming at the bottom. This information can be useful in understanding the mechanics of impact events and in predicting the location and distribution of damage caused by such events.