与叠后地震数据相比,叠前地震数据包含有更多的反映地下地层特征的信息,利用AVO(Amplitude Versus Offset,振幅随偏移距的变化)信息通过求解Zoeppritz方程的近似公式,叠前反演可直接得到反映地下岩石特征的弹性参数——密度、纵波速度和横波速度.从本质上讲,叠前地震反演是非线性的,但目前多采用线性近似方法求解,降低了地震反演的精度.本文研究基于Aki-Richards近似公式的非线性叠前反演方法,分析了引起弹性参数非线性反演误差的因素,提出了反向加权系数的方法以均衡各反演参数的系数所引起的响应差异,并把具有较强的非线性搜索能力、能够更好地求取全局最优解的量子蒙特卡罗方法引入到叠前三参数非线性反演,改善了叠前反演的精度.理论和实例试算表明:该方法计算精度较高、稳定性较好.
With the development of parallel computing technology,non-linear inversion calculation efficiency has been improving.However,for single-point search-based non-linear inversion methods,the implementation of parallel algorithms is a difficult issue.We introduce the idea of group search to the single-point search-based non-linear inversion algorithm, taking the quantum Monte Carlo method as an example for two-dimensional seismic wave velocity inversion and practical impedance inversion and test the calculation efficiency of using different node numbers.The results show the parallel algorithm in theoretical and practical data inversion is feasible and effective.The parallel algorithm has good versatility. The algorithm efficiency increases with increasing node numbers but the algorithm efficiency rate of increase gradually decreases as the node numbers increase.
