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应用地球物理  2020, Vol. 17 Issue (4): 475-488    DOI: 10.1007/s11770-020-0835-5
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叠前地震资料层间衰减估算:以阿拉伯半岛为例
Abdullah Alshangiti and Hua-Wei Zhou
1.University of Houston, Department of Earth and Atmospheric Sciences, Houston, Texas, The United States
Interval attenuation estimation from prestack seismic data: A case study from the Arabian Peninsula*
Abdullah Alshangiti and Hua-Wei Zhou
1.University of Houston, Department of Earth and Atmospheric Sciences, Houston, Texas, The United States
 全文: PDF (1927 KB)   HTML ( KB)   输出: BibTeX | EndNote (RIS)      背景资料
摘要 准确估算层间衰减 (1/Q) 值在定量解释和提高地震分辨率等方面有着广泛的应用。通常Q值可以通过测量目标层和参考层地震反射之间的谱比进行估算,但其结果会受到诸如上覆盖层非均质性等因素的影响。本文分别利用一个合成数据和一个阿拉伯半岛陆上油田实际数据,定量分析在谱比法、时空域叠前Q反演和τ-p域叠前Q反演等三种方法中上覆地层非均质性对层间Q值估算的影响。其中,合成数据 (地震道集) 来源于一个三层地层模型,且在第一层中有一个低Q值的异常体来仿真表征上覆地层的非均质性。实际数据则是来源于一个正在生产油田的、经过前期处理的成像道集。合成数据试算结果表明,上述三种方法中上覆地层低Q值的异常体对层间Q值估算均产生较大影响,但相比较而言τ-p域叠前Q反演估算Q值的误差最小 (即13.3%)。这主要归因于该方法的同时反演技术及其在τ-p域中的应用。油田实际资料试算结果也表明τ-p域叠前Q反演方法给出的层间Q值结果更加合理,而且与烃饱和碳酸盐岩储层估算的Q值相符合。
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关键词衰减   品质因子Q   上覆地层非均质性   谱比   叠前Q反演     
Abstract: Accurately estimated interval attenuation (1/Q) values have several applications, such as in quantitative interpretation and seismic resolution enhancement. Although Q values can be estimated by measuring the spectral ratio between seismic reflections from a target and a reference reflector, the results are influenced by factors such as overburden inhomogeneities. Here, we quantitatively analyze the overburden influence on interval Q estimations using the spectral ratio method, time–space domain prestack Q inversion (PSQI), and τ-p domain PSQI. We compare these three methods using a synthetic dataset and a field dataset acquired onshore the Arabian Peninsula. Synthetic seismic gathers are generated from a three-layer model with a low-Q inclusion in the first layer to mimic overburden inhomogeneity. The fi eld data are preconditioned image gathers from a producing oil fi eld. The synthetic data test shows that the small low-Q body produces a considerable error in estimated Q values. The smallest error (i.e., 13.3%) is in the τ-p domain PSQI result. Theoretically, τ-p domain PSQI could obtain more accurate Q values when there are overburden influences because of the simultaneous inversion scheme and the application in the τ-p domain. The fi eld data application also illustrates that the τ-p domain PSQI produces reasonable interval Q values. Our measured Q values are also comparable with the Q values estimated from hydrocarbon saturated carbonate reservoirs.
Key wordsAttenuation   quality factor Q   overburden inhomogeneity   spectral ratio   prestack Q inversion   
收稿日期: 2020-06-03;
基金资助:

The research was funded by the Saudi Aramco.

通讯作者: abdullah.shangiti@gmail.com     E-mail: abdullah.shangiti@gmail.com
作者简介: Abdullah Alshangiti received his BSc in Geophysics from King Abdulaziz University in 2006. In 2010, he was awarded an MSc degree with merit in Petroleum Geology and Geophysics from the University of Leeds. Abdullah worked as a seismic data processing geophysicist for the Geophysical Imaging Department at Saudi Aramco for 7 years before starting his Ph.D. program in 2017. He is currently a Ph.D. student in Geophysics at the University of Houston. His main research interests are seismic processing, inversion and attenuation estimation for quantitative interpretation, inverse Q-fi ltering.. Main and Corresponding Author: Mr. Abdullah Alshangiti, University of Houston, Department of Earth and Atmospheric Sciences, Houston, Texas, The United States (Email: abdullah.shangiti@gmail.com). Co-author: Dr. Hua-Wei Zhou, University of Houston, Department of Earth and Atmospheric Sciences, Houston, Texas, The United States (Email: hzhou@uh.edu).
引用本文:   
. 叠前地震资料层间衰减估算:以阿拉伯半岛为例[J]. 应用地球物理, 2020, 17(4): 475-488.
. Interval attenuation estimation from prestack seismic data: A case study from the Arabian Peninsula*[J]. APPLIED GEOPHYSICS, 2020, 17(4): 475-488.
 
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