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How do stress perturbations near salt bodies induce difficulty in salt imaging? Insights from a geomechanical model and salt imaging

机译:盐尸体附近的压力扰动如何诱导盐成像困难? 从地质力学模型和盐成像的见解

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摘要

Traditional methods for imaging salt bodies seldom consider near-salt stress perturbations caused by salt, and the associated velocity perturbations of seismic waves in the sediments near the salt. To demonstrate the importance of stress changes caused by the salt on accurately imaging salt bodies, in this study we develop and apply a combined method of geomechanical stress modelling and salt imaging. We simulate the stress perturbations in sediments induced by a salt sphere using a static geomechanical model, and calculate the associated velocity changes of seismic waves in the sediments by using our model stress perturbations. We use the reverse time migration and imaging method to image the salt sphere, and then analyse the imaging results of two cases including and excluding the effects of stress perturbations by the salt sphere on velocity changes of seismic waves. The results show that the near-salt velocity changes of seismic waves induced by stress perturbations near salt bodies can have a significant impact on the salt imaging. We find that when the effects of near-salt stress perturbations are ignored, the imaging of the salt sphere is clearly distorted: the salt sphere is extended vertically and becomes a salt ellipse with a vertical major axis. In contrast, when we include the effects of near-salt stress perturbations, the imaging of this salt sphere accurately matches the salt geometry and position. Thus, the near-salt stress perturbations should not be ignored in salt imaging. This study provides scientific insights for petroleum geologists and exploration geophysicists on the relationship between near-salt stress perturbations and accurate imaging of salt structures.
机译:用于成像盐体的传统方法很少考虑由盐引起的近盐胁迫扰动,以及盐附近沉积物中的地震波的相关速度扰动。为了证明盐在精确成像盐体上引起的压力变化的重要性,在本研究中,我们开发并应用了地质力学应力建模和盐成像的组合方法。我们使用静态地质力学模型模拟盐球诱导的沉积物中的应力扰动,并通过使用我们的模型应力扰动来计算沉积物中地震波的相关速度变化。我们使用反向时间迁移和成像方法来映像盐球,然后分析两种情况的成像结果,包括并排除盐球的应力扰动的影响在地震波的速度变化上。结果表明,盐体附近应激扰动引起的地震波的近盐速度变化可对盐成像产生显着影响。我们发现,当忽略近盐应激扰动的影响时,盐球的成像显然扭曲:盐球垂直延伸并使含有垂直长轴的盐椭圆形。相反,当我们包括近盐胁迫扰动的影响时,该盐球的成像精确地匹配盐几何形状和位置。因此,在盐成像中不应忽略近盐胁迫扰动。本研究为石油地质学家和勘探地球物理学家提供了科学洞察力,对近盐胁迫扰动和盐结构准确成像的关系。

著录项

  • 来源
    《Petroleum Geoscience》 |2019年第3期|共9页
  • 作者单位

    Univ Sci &

    Technol China Sch Earth &

    Space Sci Lab Seismol &

    Phys Earths Interior 96 Jinzhai Rd Hefei 230026 Anhui Peoples R China;

    Univ Chinese Acad Sci Chinese Acad Sci Coll Earth &

    Planetary Sci Key Lab Computat Geodynam Beijing 100049 Peoples R China;

    Univ Sci &

    Technol China Sch Earth &

    Space Sci Lab Seismol &

    Phys Earths Interior 96 Jinzhai Rd Hefei 230026 Anhui Peoples R China;

    Univ Chinese Acad Sci Chinese Acad Sci Coll Earth &

    Planetary Sci Key Lab Computat Geodynam Beijing 100049 Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 石油、天然气工业;
  • 关键词

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