首页> 外文会议>Annual Indonesian Petroleum Association convention and exhibition;Indonesian Petroleum Association convention and exhibition >APPLICATION OF ZERO OFFSET 2D CRS-STACK METHOD FOR LOW FOLD DATA: SYNTHETIC AND REAL DATA EXAMPLES
【24h】

APPLICATION OF ZERO OFFSET 2D CRS-STACK METHOD FOR LOW FOLD DATA: SYNTHETIC AND REAL DATA EXAMPLES

机译:零偏移二维CRS-STACK方法在低折数据中的应用:综合和真实数据示例

获取原文

摘要

Conventional seismic stack has difficulties in imaging complex subsurface structure. This could lead to produce bad seismic section, especially if the coverage of seismic data is low. Several methods have been introduced in the past years aiming to increase image quality of reflection seismic data. One of those methods is Zero Offset CRS-stack method. In this study, ZO CRS-stack method is applied to synthetic and real data examples. The effectiveness and advantages of this method is tested and compared with the results obtained from conventional stack method. As has been already known, velocity analysis is a processing step that should be done carefully in the conventional stacking method. In contrary, the CRS-stack method does not need velocity function to obtain a stack section. Only estimation of near surface velocity model is needed. The ZO CRS-stack method depends on three stacking operators, namely emergence angle, radius of NIP-waves and radius of normal waves. Velocity model is then estimated from the automatic CMP-stack. Since the stacking operator is determined from full coverage data, this method can map the reflectors in a better way, and the S/N-ratio is better than the results of conventional one, especially if the subsurface structure is complex. Several attributes are then produced as by-products, which can be used as interpretation tools. A synthetic study has been done to test the reliable of this method for complex subsurface models. After that, this method is tested to re-process a marine seismic dataset that has low fold coverage. The results of synthetic and real datashow significant improvement in the quality of stacking sections, although the coverage of data is low. Since the acquisition was carried out near the subduction zone, the geological condition is very complex. The result of conventional method unfortunately does not show continuous reflection events. In contrary, the result of ZO CRS-stack method shows better subsurface image, in which the reflectors are more continuous and the content of non-coherent noises is now decreased.
机译:传统的地震叠层难以成像复杂的地下结构。这可能会导致产生不良的地震剖面,尤其是在地震数据覆盖率较低的情况下。在过去的几年中,已经提出了几种旨在提高反射地震数据的图像质量的方法。这些方法之一是零偏移CRS堆栈方法。在这项研究中,将ZO CRS-stack方法应用于合成和真实数据示例。测试了该方法的有效性和优势,并将其与常规堆叠方法获得的结果进行了比较。众所周知,速度分析是在常规堆叠方法中应仔细进行的处理步骤。相反,CRS堆栈方法不需要速度函数即可获得堆栈截面。仅需要估计近地表速度模型。 ZO CRS叠加方法取决于三个叠加算子,即出射角,NIP波的半径和法向波的半径。然后从自动CMP堆栈估算速度模型。由于堆叠算子是从全覆盖数据中确定的,因此该方法可以更好地映射反射器,并且信噪比优于传统方法的结果,尤其是在地下结构复杂的情况下。然后产生了一些作为副产品的属性,这些属性可以用作解释工具。已经进行了综合研究,以测试该方法对复杂地下模型的可靠性。此后,对该方法进行了测试,以重新处理具有低倍覆盖率的海洋地震数据集。综合和真实数据的结果 尽管数据覆盖率较低,但显示出堆叠部分质量的显着改善。由于采集是在俯冲带附近进行的,因此地质条件非常复杂。不幸的是,常规方法的结果没有显示出连续的反射事件。相反,ZO CRS-stack方法的结果显示出更好的地下图像,其中反射器更连续,并且非相干噪声的含量现在减少了。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号