Application of AVO Characteristics Analysis and Seismic Dispersion AVO Inversion to the Carbonate Hydrocarbon Reservoirs in Region Y of the Tarim Basin, China

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2024-11-11 DOI:10.1155/2024/3034459
Hong Li, Hongwei Yin, Jinliang Tang, Pengfei Xiao
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Abstract

In recent years, breakthroughs in deep hydrocarbon exploration have been continuously achieved in the Tarim Basin of China. The Ordovician carbonate stratum has been shown to contain vast oil and gas resources. However, challenges remain in understanding the seismic response characteristics and accurately identifying the hydrocarbon reservoirs. These challenges can be attributed to factors including the significant burial depth of the target layers and complex geologic structures. To effectively support hydrocarbon exploration and resource assessment in the Tarim Basin, this study focused on the following three aspects in Region Y. First, according to the analysis of prestack amplitude versus offset (AVO) characteristics in well-adjacent seismic traces and seismic forward modeling, we demonstrated that different fluid-filled reservoirs have distinctly different AVO characteristics. This means that the hydrocarbon reservoirs in the study area can be identified by AVO inversion. Second, based on the theory that seismic waves exhibit amplitude attenuation and velocity dispersion when propagating through fluid-filled media, the seismic dispersion AVO inversion technique was developed to obtain equations for the attributes of primary (P) and shear (S) seismic wave dispersion. Finally, this technique was applied in Region Y and further verified using actual drilling data from single wells and well profiles. The application results demonstrate that hydrocarbon reservoirs can be effectively identified using this technique and provide a technical reference for reservoir identification in other areas of the Tarim Basin. The AVO characteristic analysis is the prerequisite for the successful application of this method; the key is to find accurate inversion equations and parameters to recognize the AVO response patterns in the study area.

Abstract Image

中国塔里木盆地Y区碳酸盐岩油气藏AVO特征分析和地震频散AVO反演的应用
近年来,中国塔里木盆地的深层油气勘探不断取得突破性进展。奥陶系碳酸盐岩地层蕴藏着巨大的油气资源。然而,在了解地震响应特征和准确识别油气藏方面仍存在挑战。这些挑战可归因于目标层埋藏深度大、地质构造复杂等因素。为有效支持塔里木盆地的油气勘探和资源评估,本研究在 Y 区重点开展了以下三个方面的工作。首先,根据对相邻地震道的预叠加振幅与偏移(AVO)特征的分析和地震前向建模,我们证明了不同的充满流体的储层具有明显不同的 AVO 特征。这意味着可以通过 AVO 反演确定研究区的油气藏。其次,基于地震波在充满流体的介质中传播时表现出振幅衰减和速度频散的理论,开发了地震频散反演技术,获得了地震波原波(P)和剪切波(S)频散属性方程。最后,在 Y 区应用了这一技术,并利用单井和井剖面的实际钻井数据进行了进一步验证。应用结果表明,使用该技术可有效识别油气藏,并为塔里木盆地其他地区的油气藏识别提供了技术参考。AVO特征分析是成功应用该方法的前提,关键是找到准确的反演方程和参数,以识别研究区域的AVO响应模式。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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