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Tuning, AVO, and flat-spot effects in a seismic analysis of North Sea Block F3.

机译:北海F3区块的地震分析中的调谐,AVO和平斑效应。

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摘要

Reflection seismic data from the F3 block in the Dutch North Sea exhibits many large-amplitude reflections at shallow horizons, typically categorized as "brightspots " (Schroot and Schuttenhelm, 2003), mainly because of their bright appearance. In most cases, these bright reflections show a significant "flatness" contrasting with local structural trends.;While flatspots are often easily identified in thick reservoirs, we have often occasionally observed apparent flatspot tuning effects at fluid contacts near reservoir edges and in thin reservoir beds, while only poorly understanding them. We conclude that many of the shallow large-amplitude reflections in block F3 are dominated by flatspots, and we investigate the thin-bed tuning effects that such flatspots cause as they interact with the reflection from the reservoir's upper boundary. There are two possible effects to be considered: (1) the "wedge-model" tuning effects of the flatspot and overlying brightspots, dimspots, or polarity-reversals; and (2) the stacking effects that result from possible inclusion of post-critical flatspot reflections in these shallow sands. We modeled the effects of these two phenomena for the particular stratigraphic sequence in block F3. Our results suggest that stacking of post-critical flatspot reflections can cause similar large-amplitude but flat reflections, in some cases even causing an interface expected to produce a 'dimspot' to appear as a 'brightspot'.;Analysis of NMO stretch and muting shows the likely exclusion of critical offset data in stacked output. If post-critical reflections are included in stacking, unusual results will be observed. In the North Sea case, we conclude the tuning effect was the primary reason causing for the brightness and flatness of these reflections. However, it is still important to note that care should be taken while applying muting on reflections with wide range of incidence angles and the inclusion of critical offset data may cause some spurious features in the stacked section.
机译:来自荷兰北海F3区块的反射地震数据在浅层地平线上表现出许多大幅度反射,通常归类为“亮点”(Schroot和Schuttenhelm,2003年),主要是因为它们的外观明亮。在大多数情况下,这些明亮的反射显示出明显的“平坦度”,与局部结构趋势形成鲜明对比。;虽然通常容易在较厚的储层中识别出平斑,但我们经常偶尔观察到在储层边缘附近和薄的储层中的流体接触处出现明显的平斑调谐效应,而对它们的了解却很少。我们得出的结论是,F3区块中的许多浅大振幅反射都由平斑控制,并且我们研究了这些平斑与储层上边界的反射相互作用时引起的薄层调谐效应。有两种可能的影响要考虑:(1)平坦点和上覆的亮点,暗点或极性反转的“楔形模型”调整效果; (2)可能由于在这些浅沙中包含临界后平斑反射而产生的叠加效应。我们在区块F3中对这两种现象对特定地层序列的影响进行了建模。我们的结果表明,临界后平坦点反射的叠加可能会导致类似的大振幅但平坦反射,在某些情况下甚至会导致预期产生``暗点''的界面显示为``亮点''。; NMO拉伸和静音分析显示堆叠输出中可能会排除关键偏移数据。如果堆中包括临界后反射,将观察到异常结果。在北海案例中,我们得出结论,调谐效果是导致这些反射的亮度和平坦度的主要原因。但是,仍然必须注意,在对入射角范围较广的反射进行屏蔽时应格外小心,并且包含临界偏移数据可能会在堆叠部分中造成一些杂散特征。

著录项

  • 作者

    Guo, Qiang.;

  • 作者单位

    Michigan Technological University.;

  • 授予单位 Michigan Technological University.;
  • 学科 Geophysics.
  • 学位 M.S.
  • 年度 2014
  • 页码 49 p.
  • 总页数 49
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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