“…Shale being a typical dual-porosity structure, researchers have amalgamated gas flow, deformation, matrix-fracture interaction, and heat transference to develop a dual-porosity permeability model in order to investigate the interaction between the matrix-fracture microstructure and macroscopic behavior . However, none of the above studies considered the complex features of the fracture bifurcation structure, which over time has revealed that fractures in shale’s low permeability reservoirs possess bifurcation characteristics similar to a tree network pattern. – Many researchers assumed that fractures resembled a forked symmetric fracture network through referral to fracture fractal theory and to characterize the complex bifurcated fracture network structure based on simple mathematical iteration. ,, However, the above research was constructed on a static fractal dimension, which was inconsistent with the actual situation. Porosity varied during the shale gas production process under the influence of various factors, indicating that the pore’s heterogeneity, including pore size, also differed and was not constant; therefore, the fractal dimension characterizing the pore’s heterogeneity should reflect change.…”