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An accurate formulation of log-stretch dip moveout in the frequency-wavenumber domain

机译:波数域中对数-拉伸倾角偏移的精确公式

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摘要

In this paper, a new and accurate log-stretch F-K DMO formulation was presented. The result is identical to the one of Gardner (1991) except for a sign difference on the phase shift, which is caused by the definition of the 2-D Fourier transform. The derivation of the new DMO operator was based on the correct DMO relationships presented in Black et al. (1993), which take the repositioning of the midpoint into consideration. These correct DMO relationships, in common with Gardner's method, are parametric representations of the DMO process, but with better physical insight to the process than Gardner's method. No approximation was introduced during the derivation. Therefore, the new log-stretch DMO is accurate and can adequately handle steeply dipping reflectors. The final form of the new DMO is also identical to that of Liner (1990) with respect to phase shift, while the amplitude factor is different. The numerical impulse responses show that the difference in results between the new DMO and Liner's DMO is subtle. However, our new DMO operator should produce slightly stronger amplitudes for steep reflectors because Liner's DMO amplitude factor is always less than ours and decreases as the time dip (k/Ω) increases. The philosophy of our basic derivation is the same as Bale and Jakubowicz (1987). But the starting point is different: Bale and Jakubowicz start from the conventional NMO/DMO equation as did Hale (1984) while we start from the new DMO relationships from Black et al. (1993) who corrected the subtle flaw in Hale's DMO formulation, i.e., the repositioning of the midpoint. Therefore, we conclude that the subtle flaw of Hale's derivation is largely responsible for the inaccurate DMO impulse responses of Bale's DMO. We do not have a satisfactory explanation to why Hale's F-K DMO operator is correct although it was based on two inaccurate assumptions: First, the midpoint was not repositioned, i.e. x_0 = x_n. Second, the time relationship before and after DMO is not strictly correct: t_0 = t_nA. It might be that these two approximations (errors) somehow counteract each other in the F-K domain to make the final result correct. But they do not cancel each other in the log-stretch F-K domain. They do not even describe the DMO elliptical responses in the x-t domain in the first place.
机译:在本文中,提出了一种新的,准确的对数拉伸F-K DMO配方。结果与Gardner(1991)的结果相同,只是相移的符号差异是由二维傅立叶变换的定义引起的。新的DMO算子的派生是基于Black等人提出的正确的DMO关系。 (1993),其中考虑了中点的重新定位。与Gardner的方法相同,这些正确的DMO关系是DMO过程的参数表示,但是与Gardner的方法相比,它们对过程具有更好的物理洞察力。在推导过程中未引入任何近似值。因此,新的对数拉伸DMO是准确的,可以充分处理陡峭倾斜的反射镜。关于相移,新的DMO的最终形式也与Liner(1990)相同,而幅度因子却不同。数值冲激响应表明,新的DMO与Liner的DMO之间的结果差异很小。但是,我们的新DMO运算符应该为陡峭的反射器产生稍强的幅度,因为Liner的DMO幅度因数始终小于我们的幅度因数,并且随着时间骤降(k /Ω)的增加而减小。我们基本推导的哲学与Bale和Jakubowicz(1987)相同。但是起点是不同的:Bale和Jakubowicz像Hale(1984)一样从传统的NMO / DMO方程开始,而我们从Black等人的新DMO关系开始。 (1993年),他纠正了黑尔DMO公式中的细微缺陷,即中点的重新定位。因此,我们得出的结论是,Hale派生的细微缺陷在很大程度上是Bale DMO的DMO脉冲响应不准确的原因。尽管Hale的F-K DMO算子基于两个不正确的假设,但我们对它为什么是正确的没有令人满意的解释:首先,中点没有重新定位,即x_0 = x_n。其次,DMO前后的时间关系不是严格正确的:t_0 = t_nA。这两个近似值(错误)可能以某种方式在F-K域中相互抵消,以使最终结果正确。但是它们在对数拉伸F-K域中不会互相抵消。他们甚至根本没有描述x-t域中的DMO椭圆响应。

著录项

  • 来源
    《Geophysics》 |1996年第3期|p.815-820|共6页
  • 作者单位

    CSIRO Division of Exploration and Mining, P.O. Box 883, Kenmore, QLD 4069, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

  • 入库时间 2022-08-18 00:20:10

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