Study of Converted-Wave Modeling: AVO Application for Shallow Gas Models

N. C. Viony, Wahyu Triyoso
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引用次数: 2

Abstract

The application of converted-wave seismic method in hydrocarbon exploration has increased significantly. Since the conventional seismic ceases to provide an adequate result in complex geology area and it provides an ambiguous brightspot response. The main principle is that an incident P-wave produces reflected and converted P and SV wave when the downgoing P-wave impinges on an interface. Converted-wave seismic uses the multicomponent receiver that records both of vertical component and horizontal component. The vertical component is assumed to correspond to the compressional PP wave and the horizontal correspond to the PS converted-wave. In this research, a synthetic model with the shallow gas and the salt dome below are constructed. The purpose of this study is to analyze the brightspot due to the presence of shallow gas and its effect to the quality of PP and PS wave reflection below the gas zone. To achieve the goal, both vertical and horizontal seismic data processing are performed. In horizontal data processing, the best gamma function (Vp/Vs) value is estimated to produce the better and reliable image. The result shows that the brightspot response in conventional data doesn’t exist in converted-wave data and the imaging below the gas zone in converted-wave data is better than the conventional due to the attenuation and diffraction effect that caused by gas column. Processing is followed by AVO analysis to compare the AVO response of PP and PS data in characterizing gas reservoir. Both PP and PS AVO curve shows the consistency with synthetic AVO from well data. Gas reservoir is a class 1 AVO anomaly with positive intercept and negative gradient on PP data. However, PS AVO curve does not refer any anomaly. It is because S-wave is not sensitive to the existence of rock saturant.
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转换波建模研究:AVO在浅层天然气模型中的应用
转换波地震方法在油气勘探中的应用日益增多。由于常规地震在复杂地质区域不能提供充分的结果,并且提供模糊的亮点响应。主要原理是入射的纵波在向下的纵波撞击界面时产生反射和转换的P波和SV波。转换波地震采用多分量接收器,同时记录垂直分量和水平分量。垂直分量对应于压缩PP波,水平分量对应于PS转换波。在本研究中,建立了含浅层气及其下方盐丘的综合模型。本研究的目的是分析由于浅层气的存在而产生的亮点及其对气区下方PP波和PS波反射质量的影响。为了实现这一目标,对垂直和水平地震数据进行了处理。在水平数据处理中,估计出最佳的伽马函数(Vp/Vs)值,以产生更好、更可靠的图像。结果表明,转换波数据中不存在常规数据中的亮点响应,并且由于气柱的衰减和衍射效应,转换波数据中气带下方的成像优于常规数据。处理后进行AVO分析,比较PP和PS资料在气藏表征中的AVO响应。PP和PS AVO曲线与井资料合成AVO曲线一致。气藏在PP数据上为正截距、负梯度的1类AVO异常。然而,PS AVO曲线没有任何异常。这是因为s波对饱和岩的存在不敏感。
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