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本文在过去工作的基础上,继续讨论了鄂尔多斯地块运动特征,并从力源和地震活动相关角度提出,在估计该地块地震趋势时,应将大华北以至日本海沟地震活动水平与其联系起来。
Based on the past work, the paper discusses the movement characteristics of the Ordos block and puts forward from the point of view of the relationship between the source of force and the seismic activity. When estimating the seismic tendency of the block, the seismic activity level of the Great Northern China-Japan trench should be linked with it .