The invention discloses a three-
dimensional modeling method for a geological
mass. The method comprises the steps that a geological
mass model to be constructed and geometric description of spatial
fissure surfaces are given; for the geological
mass model, a trace formed by boundary surfaces and the
fissure surfaces is solved, and edges are obtained; the edges are subjected to regularization
processing, directed rings are formed after a boundary operator is utilized and search is performed, and directed surfaces are formed based on property judgment on the directed rings and
inclusion relation judgment on the directed rings; the directed surfaces are subjected to regularization
processing, directed shells are formed after the boundary operator is utilized and search is performed, and directed bodies are formed based on property judgment on the directed shells and
inclusion relation judgment on the directed shells; and all the formed directed bodies are subjected to mass topological check and mass volume sum check. According to the method, it is not needed to introduce any artificial
hypothesis, the geological mass with arbitrarily complicated space is formed completely according to actual geologic structure surface characteristics, and therefore the method has important application value in
engineering practice and has positive theoretical significance for development of a non-continuum mechanic numerical method.