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基于简化地震模型， 根据发震断层的倾角、地震震源深度这两个参数， 提出一种简便的定量化确定潜在震源区边界的方法， 并对本方法的应用进行了具体说明。该方法物理意义明确， 简单直观， 便于掌握应用
Based on the simplified seismic model, a simple method of quantitatively determining the boundary of potential source region is proposed based on the two parameters of seismogenic fault dip and seismic focal depth. The application of this method is described in detail. The physical meaning of the method is clear, simple and intuitive, easy to grasp the application