【一般講演】 岩盤工学／ 資源開発技術

[2409-17-07] (学生発表：修士課程)全波形逆解析による震源時間関数の推定

○于 小千¹、三ヶ田 均¹、武川 順一¹、徐 世博¹ (1. 京都大学)

司会：佐藤晃（熊本大学）

キーワード：震源時間関数、全波形逆解析、逆伝播

Earthquake source inversion is essential in earthquake physics and applied studies in earthquake engineering. Accurate source time functions can be estimated by the full-waveform inversion (FWI) approach through the backpropagation algorithm in a three-dimensional elastic case. The residual wavefield, i.e. the differences between observed and simulated wavefields, are back-propagated in time from the receiver to estimate the distribution of gradient of the L2-norm error function to minimize the total error in the backpropagated strain wavefield. On the basis of this method, an iterative process of the conjugate gradient method is conducted with the line search to find an optimum step length of an update vector in the parameter space. The results show that the prescribed source time function is well estimated, and the error function converges within several iteration steps. For the sources of high complexity, this approach can be applied to describe the detailed rapture process and the asperity of earthquakes.