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采用应变梯度理论，解释了地震包体的形成，给出了包体宽度w＝2πl，其中l是岩石内部特征长度．
Using the theory of strain gradient, the formation of seismic inclusions is explained, and the width of the inclusions is given as w = 2πl, where l is the internal characteristic length of the rock.