The leftover coal in the Lijiahao Coal Mine is easy to spontaneously ignite. During the mining process of the shallow buried coal seam, the overlying fissure network in the goaf easily penetrates the goaf of the upper and lower coal seams and continues to the surface, resulting in air leakage in the mine and the hidden danger of spontaneous combustion of the leftover coal protrude. Through physical model experiments, this paper simulates the overburden structure and fracture development characteristics of Lijiahao shallow buried coal seam mining, and uses fractal dimension and image processing technology to quantitatively describe the generation and development process of overburden cracks. Combined with the classical mechanical model of "fixed beam" and "masonry beam", the causes of fracture dynamic evolution are analyzed. The results show that due to the existence of key layers between the coal seams, the stress evolution in the upper and lower seams of the key layer is not synchronised, with only small changes in stress in the upper layer before the key layer is broken, and the stress evolution in the lower layer is similar to that of a single coal seam mining. When the key layer is broken, the stress of the upper and lower rock layers will change dramatically; the fracture of the key layer also has a significant impact on the evolution of fracture fractal dimension, length, and area. The fractal dimension of the fissures rised from 1.4 to 1.5, the total area of fissures is increased from 16638 pixels to 17707 pixels, and the total length is increased from 2217 pixels to 3071 pixels; after the main key layer of the overlying rock is broken, the fractal dimension of the fissures is reduced from 1.56 to 1.5, and the total area of fissures is reduced from 31451 pixels to 29089 pixels, the total length has increased from 5657 pixels to 6619 pixels; before the key layer between the coal seams is broken, it will be suspended to form a "fixed beam". After the first break, the broken rock above it will settle synchronously until the rock blocks form a hinged structure and then collapse. After the fall stops, the key layer periodically breaks to form a "masonry beam" structure, and the overlying stratum settles synchronously. Due to the good integrity of the overlying strata, the secondary development of cracks is relatively moderate.