Inversion of sparse spike impedance is the most popular method for wave impedance inversion.
稀疏脉冲阻抗反演是目前最流行应用的波阻抗反演方法。
Constrained sparse spike inversion is conducted to predict the general distribution of reservoirs before GI, and the results including wavelet and 3D acoustic impedance(AI) can be used later.
在执行地质统计学反演前，首先应用稀疏脉冲约束反演，了解储层的大致分布，以求取子波和水平变差函数。
Constrained sparse spike inversion is conducted to predict the general distribution of reservoirs before GI, and the results including wavelet and 3D acoustic impedance(AI) can be used later.
在执行地质统计学反演前，首先应用稀疏脉冲约束反演，了解储层的大致分布，以求取子波和水平变差函数。
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