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假如你刚加入了一个新的专家组或新的公司,要你对某个地区进行评价,资料包括地震、测井和波阻抗数据体。你用波阻抗数据体作些什么呢? 它是怎样产生的?它提供了什么特定信息?存在哪些陷阱和人为因素?你怎样在为地震资料设计的工作站上解释波阻抗数据集呢?怎样对你的主管部门汇报你的成果?如何进行合理的分析?请往下读。地震数据到波阻抗(AI)的反演是一个迅速发展的领域,这主要是由于解释波阻抗数据的简易性和精确性决定的。因为反演这个术语在不同地学分支内有不同的含义,所以该术语可能非常混乱。本文将集中对叠后地震道到波阻抗数据的反演进行讨论。也正是在这个局限的邻域内,我们对当今市场上过多的各种反演方法程序进行比较,最多也只能艰难地确定你的AI
If you have just joined a new group of experts or a new company, ask you to evaluate a certain area, including seismic, logging and wave impedance data volume. What do you do with wave impedance data bodies, how does it happen, what specific information does it provide, what pitfalls and artifacts exist, and how do you interpret wave impedance data sets at workstations designed for seismic data? How does your department report your achievements? How do you make a reasonable analysis? Please read on. The inversion of seismic data to wave impedance (AI) is a rapidly evolving area, mainly due to the simplicity and accuracy of interpreting wave impedance data. Because the term inversion has different meanings in different geography branches, the term can be very confusing. This article will focus on the post-stack seismic trace to the impedance data inversion is discussed. It is also within this confined neighborhood that we compare the various over-the-top inversion methods available on the market today, at the very least, to determine your AI with a hard time