摘要
利用广义反射、透射系数矩阵和离散波数方法 ,计算了水平分层花岗岩介质中近场 (十几公里 )范围内三次地下爆炸的地表粒子速度垂直分量波形 ,并通过对实测波形的拟合 ,得到了地下爆炸激发的地震震源函数。
Vertical surface particle velocity waveforms recorded within 15km from three underground explosion centers were simulated.Effective source functions were obtained from recorded and calculated waveform.
引文
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