Maximum co-seismic displacement is one of the most important parameter to understand earthquake rupture mechanism and evaluate fault earthquake risk.
最大位移是认识地震破裂机理和断层未来地震危险性的最重要参数之一。
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Based on the concept of the change in co-seismic Coulomb stress resulting from the interaction of faults, the earthquake trigging and delaying effects of fault interaction are proposed in this paper.
In the prediction of lateral reservoir variations, co-Krige method is used to combine seismic inversion results and original log data to form an integrated geological model.