从近地表到油藏及以下的q补偿:阿布扎比陆上案例研究

Cara Smith, P. Vasilyev, A. Glushchenko, D. Zarubov
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摘要

阿布扎比地区对地震数据定量解释(QI)的兴趣持续稳步增长,创建可反转地震数据的目标正在推动地面地震数据处理工作流程的发展,重点是在整个处理过程(成像前、成像中和成像后)中更详细、更彻底地处理振幅和相位。为了在整个勘探过程中实现紧密的井间联系,并确保数据适用于解释目的,零相位和小波稳定性(以及在地球模型构建过程中使用井信息)是深度成像地震处理工作流程中的关键阶段。精确的振幅与偏移和方位角处理也需要反演研究。在本文中,我们提出了一种工作流程,在处理流程的早期将地球物理和地质上可靠的3D变量q场构建到地球模型中,从而可以更完整地处理地下q效应,而不会增加项目周转时间。本案例研究表明,数据驱动的空间可变q场与Kirchhoff叠前深度偏移相结合,有效地补偿了幅度和相位效应,与应用恒定的预偏移q补偿(以前被认为适用于这种低起伏区域)相比,提供了具有改进事件连续性和更好处理噪声的宽带图像。通过将可变q场校准到可用的测井曲线和近地表信息,并确保地球模型中不同的地球物理参数都适当地耦合在一起,可以获得增强图像,然后只需最小的频谱整形或偏移后的剩余相位校正。基于射线的q层析成像工作流程允许在适合深度成像的高分辨率地球模型中,迭代3D更新以及耦合的地下属性(如各向异性和速度)。可靠的相位稳定性、更高的分辨率、更宽的可用带宽和改进的幅度保存是这种整体方法的关键目标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Q-Compensation from Near Surface to Reservoir and Below: Case Study from Onshore Abu Dhabi
Interest in quantitative interpretation (QI) of seismic data in the Abu Dhabi region continues to steadily increase, and the objective of creating inversion-ready seismic data is driving evolution of the surface seismic data processing workflows to focus on more detailed and thorough handling of the amplitude and phase throughout processing (pre-, during, and post-imaging). To achieve close well ties across the survey and to ensure the data is suitable for interpretation purposes, zero-phasing and wavelet stability (along with using well information during earth model building) are key stages in the depth imaging seismic processing workflow. Accurate amplitude with offset and azimuth handling is also required for inversion studies. In this paper, we propose a workflow where a geophysically and geologically credible, 3D variable Q-field is built into the earth model early in the processing flow, allowing a more complete approach to handling the Q-effects of the subsurface without increasing project turnaround time. This case study shows that a data-driven spatially variable Q-field combined with Kirchhoff Pre-Stack Depth migration compensates effectively for both amplitude and phase effects, providing a broadband image with improved event continuity and better handling of noise compared with applying a constant pre-migration Q-compensation (which was previously thought to be suitable for this low-relief region). By calibrating the variable Q-field to available well logs and near surface information, and ensuring that the different geophysical parameters in the earth model are all suitably coupled, an enhanced image is achieved which then requires minimal spectral shaping or residual phase corrections post migration. Ray-based Q-tomography workflows allow iterative 3D updates alongside coupled subsurface properties like anisotropy and velocity, within a high-resolution Earth model suitable for depth imaging. Reliable phase stability, higher resolution, broader useable bandwidth and improved amplitude preservation are key targets of this holistic approach.
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