The invention relates to a method for predicting a current
ground temperature field of a broken basin. The method comprises the following steps: firstly, acquiring a
ground temperature gradient mean value of a well point stable section in a research area, and dividing the research area into a plurality of sub-areas according to parameters such as a stratum compaction coefficient; then, establishing a preliminary prediction model between the
ground temperature gradient and the weighted average value of the mourphy
surface depth, the substrate depth and the stratum
thermal conductivity in each sub-region; and systematically screening out a well location with a relatively high ground
temperature gradient by identifying the residual error of the preliminary prediction model, and further quantitatively analyzing the enhancement effect of deep and large fractures on a ground temperature field, namely determining the
temperature control influence range of each fracture based on three-dimensional seismic data, calculating the distance between the well location and the fracture, and obtaining the enhancement efficiency coefficient of the fracture through
linear regression. Correcting the preliminary model to obtain a final prediction model; and finally, based on the regional basic map and the final model, performing gridding calculation and generating a high-precision ground
temperature gradient distribution map.