This application discloses a method for predicting the strong
seismic stability of high mountains, relating to the field of rock
mass engineering geological dynamics. The method includes: constructing a two-dimensional model of the target mountain; determining the sliding surface of the two-dimensional model; dividing the two-dimensional model into multiple sliding body elements based on the sliding surface; constructing a permissible sliding
velocity vector field for the two-dimensional model; calculating the external force power and
internal energy dissipation of the two-dimensional model based on the permissible sliding
velocity vector field and the internal structural
surface strength parameters of the two-dimensional model after freeze-thaw cycle degradation; and predicting the strong
seismic stability of the target mountain based on the external force power and the
internal energy dissipation. This method solves the problem that existing
limit analysis upper bound methods generally do not fully consider the synergistic effect of freeze-thaw cycles and
fissure water seepage, leading to difficulties in accurately predicting the strong
seismic stability of high mountains.