Towards broadband multicomponent seismology and practical iterated inversion

走向宽带多分量地震学和实用迭代反演

• 批准号: 461179-2013
• 负责人: Innanen, Kristopher
• 金额: $ 32.05万
• 依托单位: University of Calgary
• 依托单位国家: 加拿大
• 项目类别: Collaborative Research and Development Grants
• 财政年份: 2016
• 资助国家: 加拿大
• 起止时间: 2016-01-01 至 2017-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=597860
• 关键词: Towards; broadband; multicomponent; seismology; practical

Seismic images provide the best possible views of the earth below its surface; but, despite an 80 year history, they are still far from optimal. Today, seismic computational techniques are transitioning from a standard methodology (SM), which incorporates an evolved blend of physical theory and practical experience, to the very modern full-waveform inversion (FWI) that is much more firmly rooted in mathematical physics. However, this transition is hindered by insufficient low-frequency content in seismic data, by the inherently unknown seismic source waveform, by incompletely understood physics, and by the extreme computational effort required. As a consequence, SM is the dominant approach while FWI is rarely attempted outside of dedicated research labs. SM uses a sophisticated data processing sequence to create a reflectivity image of the subsurface. Then, incorporating well information, an inversion process converts the reflectivity image to earth properties such as impedance (density times velocity). FWI is a fundamentally iterative process that converges on an impedance model by minimizing the difference between real and predicted seismic data. FWI never creates a reflectivity image and does not use well control while SM does not predict synthetic data and is not iterated. We will create a new class of seismic inversion methods for multicomponent data that combines the most robust features of SM with the most promising concepts from FWI. From SM, we will retain most of the data processing steps, the creation of a reflectivity image, and the matching to well control. The latter facilitates the source waveform estimation and provides the needed low frequency information. From FWI, we will incorporate the concepts of iteration, data modelling (prediction), and imaging of the data residual. The proposed approach, which we call IMMI (Iterated Modelling, Migration, and Inversion), will produce estimates of subsurface properties that both match measurements in wells and also predict most features in the recorded seismic data. Such estimates should be much more reliable than those presently achieved by SM. This will have significant benefits to resource exploration and to subsurface environmental studies.

地震图像提供了地表下地球的最佳视图；但是，尽管有80年的历史，它们仍远未达到最佳状态。如今，地震计算技术正在从标准方法（SM）向现代全波形反演（FWI）过渡，SM是物理理论和实践经验的进化融合，而FWI则更牢固地植根于数学物理。然而，由于地震数据中低频内容不足、固有的未知震源波形、不完全了解的物理特性以及所需的极端计算工作量，这种转变受到了阻碍。因此，SM是主要的方法，而FWI很少在专门的研究实验室之外尝试。SM使用复杂的数据处理序列来创建地下反射率图像。然后，结合井信息，反演过程将反射率图像转换为地球属性，如阻抗（密度乘以速度）。FWI基本上是一个迭代过程，通过最小化实际地震数据与预测地震数据之间的差异，收敛于阻抗模型。FWI从不生成反射率图像，也不使用井控，而SM不预测合成数据，也不迭代。我们将为多分量数据创建一类新的地震反演方法，将SM最强大的特征与FWI最有前途的概念相结合。从SM中，我们将保留大部分数据处理步骤，创建反射率图像，并与井控相匹配。后者便于源波形估计，并提供所需的低频信息。从FWI，我们将纳入迭代，数据建模（预测）和数据残差成像的概念。我们提出的方法称为IMMI（迭代建模、迁移和反演），它将产生与井中测量结果相匹配的地下属性估计，并预测记录地震数据中的大多数特征。这样的估计应该比目前由SM得出的估计可靠得多。这将对资源勘探和地下环境研究有重大的好处。