PSDM处理对阿布扎比东岸低起伏构造的价值

Thuraya Al Ghafri, Youngtak Seo, Jinhui Liu, Dong-Oh Kim, Ren Aijing, K. Belaid, Zhao Mingqiu, Jia Wenrui
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引用次数: 0

摘要

阿拉伯湾是低起伏地质构造的多产地,然而,它们的定义和成像通常是一个真正的挑战。人们也普遍认为,低起伏结构不会从叠前深度偏移(PSDM)中受益,而叠前时间偏移(PSTM)是最终需要的过程。因此,PSTM经常被应用于这些低起伏构造的成像。尽管如此,我们最近的3D PSDM处理工作表明,这种看法并不总是正确的,并且证明了PSDM确实可以为低浮雕结构增加显著的价值。各向异性PSDM (APSDM)工作流程经过精心设计,并精心应用于位于阿联酋阿布扎比海岸的一个非常低的浮雕结构。该三维各向异性PSDM处理的主要目标是:以更高的分辨率获得准确、清晰的深度结构图像。缓解和解决现有井的观测深度不确定性。增强断层结构和成像。分析各向异性速度,建立可靠的深度成像速度模型。解释深度和时间域的方位角体积。所设计的处理流程主要包括以下五个阶段:采用幅度保持原理进行采集预处理和残差噪声抑制。利用现有的井数据、解释的层位以及应用VTI全方位和多方位速度层析成像过程来建立和更新速度。利用Kirchhoff PSDM在OVT(偏移矢量贴图)域进行深度成像。除方位各向异性分析和最终深度检查外,还对剩余层间倍数进行偏移后处理和噪声衰减。后堆栈处理采集足迹去除和信噪比(S/N)的提高。应该指出的是,所有加工步骤的最佳加工参数的选择都是在执行了密集的测试和严格的QC/QA程序之后完成的。三维各向异性PSDM处理和随后的三维地震数据解释的主要结果和发现总结如下:与现有井的PSDM相比,PSDM具有更小的深度不确定性。然而,根据PSDM之后最近进行的钻井活动的结果,新井位的深度不确定性仍然存在。建立了可靠的深度成像速度模型。这是在对各向同性速度模型进行了12次层析迭代,并对各向异性更新和VTI方位速度层析进行了4次迭代后得出的结论。一些低起伏构造在PSDM中比在PSTM中定义得更好。一些目标层的地震连续性得到了改善。由于频率含量有限,地震分辨率降低。断层成像在某些位置得到了改进。
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Value of PSDM Processing on Low Relief Structure in East Onshore Abu Dhabi
The Arabian Gulf is prolific of low relief geological structures, however, their definition and imaging present in general a genuine challenge. It is also commonly understood that low relief structures won't benefit from Pre-Stack Depth Migration (PSDM) whereas, Pre-Stack Time Migration (PSTM) is the ultimate required process. Thus, PSTM is frequently applied for the imaging of these low relief structures. Nonetheless, our recent 3D PSDM processing work has demonstrated that this perception is not all the time correct and has proved that PSDM can indeed add significant value to low relief structures. An Anisotropic PSDM (APSDM) workflow was carefully designed and meticulously applied on a very low relief structure located onshore Abu Dhabi –UAE. The main objectives of this 3D Anisotropic PSDM processing were established as follows: Achieve an accurate & clearer depth structure image with higher resolution.Mitigate & address the observed depth uncertainties at the existing wells.Enhance the faults architecture & imaging.Analyze anisotropic velocity & build a reliable velocity model for depth imaging.Interpret azimuth volumes in depth & time domains. The designed processing workflow consisted of the following main five stages: Gathers pre-conditioning and residual noise attenuation adopting the principle of amplitude preservation.Velocity building & updating using available well data, interpreted horizons and applying VTI full azimuth and multi azimuth velocity tomography processes.Depth imaging using Kirchhoff PSDM in OVT (Offset Vector Tile) domain.Post migration processing for residual inter-bed multiples & noise attenuation in addition to azimuthal anisotropy analysis and final depth-tie examination.Post stack processing for acquisition foot print removal and signal to noise ratio (S/N) enhancement. It should be noted that the selection of the optimum processing parameters at all the processing steps was done after the implementation of an intensive testing & rigorous QC/QA procedures. The main results and findings revealed by the 3D Anisotropic PSDM processing and the subsequent 3D seismic data interpretation are summarized as follows: PSDM shows less depth uncertainty compared to PSTM at existing wells. However, based on the results of recent drilling activities which have been conducted after PSDM, depth uncertainty at new well locations still exists.Reliable velocity model was built for depth imaging. This was established after 12 tomography iterations carried out for the isotropic velocity model and four iterations of anisotropy updates and VTI azimuthal velocity tomography.Some low relief structures are better defined in PSDM than PSTM.Seismic continuity of some target levels has been improved.Seismic resolution is degraded due to the limited frequency content.Fault imaging has been improved at some locations.
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