波节面
The results are as follows: The directivity of source time functions retrieved from P-and S-waves indicate that the nodal plane striking 199 ° is the fault plane, and that the earthquake ruptured unilaterally from the northeast to the southwest.
从P波和S波提取的震源时间函数的方向性效应都清楚地表明:走向为199°的节面为断层面,地震是从东北向西南方向的单侧破裂。
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