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建立了地震反卷积信号处理的状态空间模型,应用最优平滑理论、卡尔曼滤波及最小方差准则,推导出了确定地层反射系数的计算公式,并利用修正的Fadeev算法和Systolic阵列进行了并行实现
The state space model of seismic deconvolution signal processing is established. Based on the optimal smoothing theory, Kalman filtering and minimum variance criterion, the formula to determine the formation reflection coefficient is deduced. The modified Fadeev algorithm and Systolic array are used to parallelize achieve