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New imaging and filtering methods: Primary only imaging condition and interferometric migration.

机译:新的成像和过滤方法:仅主要成像条件和干涉迁移。

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摘要

Two new imaging and filtering methods are formulated and applied to both synthetic and field data. One of the methods, denoted as primary only imaging condition (POIC) migration, discriminates primary reflections from multiple reflections and migrates only the primary reflections using the prestack wavepath migration (WM). The other method is interferometric migration (IM), which can redatum the traces below salt without knowing the velocity model in or above the salt body.; The POIC migration and its practical implementations are presented and applied to both two-dimensional (2-D) synthetic and field marine data for multiple suppression. The key idea is that both the take-off and incidence angles are picked from the seismic data and rays are traced from both the source and the receiver positions along these picked angles. An event is a primary reflection if the intersection point of the rays has a reflection traveltime equal to the observed traveltime. In contrast, an event is a multiple reflection if the intersection point has a reflection traveltime different from the observed traveltime. Test results show that POIC is effective in suppressing the migration artifacts generated by multiple energy in the far-offset data and appears to perform better than the traditional Radon multiple attenuation method in the field test.; The POIC method predicts the multiples in the far-offsets and guides the muting of near-offset multiples in the tau - p domain with a parabolic Radon transform. Synthetic results indicate that the approach is effective in separating the primary reflections from multiple events in the near offset traces.; The POIC method is further combined with the wave-equation based reverse-time datuming (RTD) to better suppress multiples and image the reflectivity distribution below the salt body. The RTD method can extrapolate both primaries and multiples to locations beneath the salt so that the ray-based POIC can suppress multiples in the subsalt areas with a relatively simple velocity model. Synthetic results show that the hybrid approach can eliminate most of multiple artifacts in the subsalt image.; The interferometric migration and the reduced time migration (RTM) are developed and applied to both synthetic and field CDP data. Both IM and RTM use the natural arrival times associated with the reflections from a reference reflector which can be picked from the data. The RTM shifts the data with the time difference between the calculated and natural arrival times of a reference reflection, while IM extrapolates the data to the reference datum with the natural arrival times and then migrates the redatumed data below salt. (Abstract shortened by UMI.)
机译:制定了两种新的成像和滤波方法,并将其应用于合成和现场数据。一种方法称为“仅主要成像条件”(POIC)迁移,它使用叠前波径迁移(WM)来将主要反射与多次反射区分开,并仅迁移主要反射。另一种方法是干涉迁移法(IM),它可以重新计算盐以下的迹线,而无需知道盐体内或盐体内的速度模型。介绍了POIC迁移及其实际实现,并将其应用于二维(2-D)合成和野外海洋数据以进行多重抑制。关键思想是,从地震数据中选取起飞角和入射角,并沿这些拾取角从源位置和接收器位置追踪射线。如果光线的交点的反射传播时间等于观察到的传播时间,则事件是主要反射。相反,如果相交点的反射传播时间不同于观察到的传播时间,则事件为多重反射。测试结果表明,POIC可以有效地抑制由多种能量在远距偏移数据中产生的迁移伪影,并且在现场测试中表现出比传统Radon多重衰减方法更好的性能。 POIC方法通过抛物线Radon变换预测远偏移的倍数,并指导tau-p域中近偏移倍数的静噪。综合结果表明,该方法可有效地将主反射与近偏移迹线中的多个事件分开。 POIC方法还与基于波方程的逆时基准(RTD)相结合,可以更好地抑制倍数,并成像盐体下方的反射率分布。 RTD方法可以将原始和倍数外推到盐下的位置,以便基于射线的POIC可以使用相对简单的速度模型来抑制盐下区域的倍数。综合结果表明,混合方法可以消除盐下图像中的大部分伪影。干涉式偏移和减少时间偏移(RTM)已开发并应用于合成和现场CDP数据。 IM和RTM都使用与来自参考反射器的反射相关联的自然到达时间,可以从数据中获取该自然到达时间。 RTM使用参考反射的计算出的和自然到达时间之间的时间差来移动数据,而IM用自然到达时间将数据外推到参考基准,然后将重定的数据迁移到盐以下。 (摘要由UMI缩短。)

著录项

  • 作者

    Zhou, Min.;

  • 作者单位

    The University of Utah.;

  • 授予单位 The University of Utah.;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 86 p.
  • 总页数 86
  • 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 2022-08-17 11:42:26

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