ZHANG Xichen, HAN Ruidong, DU Changjiang, LI Lei, CHEN Maoshan, FENG Jiameng
Using fault-sensitive attributes to identify faults is limited in accuracy and applicability, mainly able to identify major large-scale faults. As medium and small-scale faults lack sufficient resolution and continuity, the predicted number of faults is inaccurate. The credibility of predicting faults solely relying on a single attribute is relatively lower. In addition, for a long time, fault interpretation has been mainly done manually, seriously affecting working efficiency. To overcome the limitations of a single method, thus identifying more fault layers, improving the resolution and continuity of fault prediction, and eliminating the “double boundary” effect, this paper creates a high-precision artificial intelligence fault prediction process to gradually improve the accuracy and efficiency of fault interpretation. Firstly, post-stack seismic data preprocessing is carried out to improve the quality of original seismic data and establish a foundation for generating high-precision fault attributes. Secondly, artificial intelligence fault prediction is carried out to further improve the prediction accuracy and process the artificial intelligence prediction results in the “fault enhancement-skeletonization-ant body” way. Again, multi-attribute fusion is utilized to enrich multi-scale fault information. Finally, with high-precision fault prediction results and intelligent technology, the efficiency of fault interpretation is improved. The high-precision artificial intelligence fault prediction process was applied to the actual data of Zone X in the Bohai Bay Basin, and the results showed that the profile normal faults are mainly composed of stepped and Y-shaped combinations. Most of them are SE orientation and form simultaneously with the fault depression. The dominant orientation of the fault on the plane is NE, and forms a comb-like combination with secondary faults in the near SN direction, indicating that the area may have undergone sinistral strike slip while deforming extensionally.