The rupture surface is to NNE, similar to gradient belt of focal depth, gradient belt of crustal deformation, isoseisms and extended direction of earthquakes.

 
  • 伽師強震群的破裂斷層面為北東向,與震源深度梯度變化帶、地殼接觸變形梯度變化帶、等烈度線(xiàn)以及地震擴展方向吻合;
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