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首页> 外文期刊>Doklady Earth Sciences >Intensity of Scattered Waves: A New Seismic Criterion for Predicting Filtration-Capacity Properties of an Oil-Saturated Reservoir
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Intensity of Scattered Waves: A New Seismic Criterion for Predicting Filtration-Capacity Properties of an Oil-Saturated Reservoir

机译:的散射波强度:预测油饱和油藏的过滤能力的新地震判据

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1. The oil fields of eastern Siberia are usually confined to certain local heterogeneities of the lithologi-cal replacement type, as opposed to classical structures. Such zones are generally characterized by a high degree of fracturing. Therefore, they produce not only reflected waves, but also sufficiently intense scattered wave fields in seismic records. The seismic wave field in such zones can be presented as a superimposi-tion of reflected and scattered/diffracted waves. It is natural that both types of the wave field should be studied in order to scrutinize the reservoir structure, because the two wave fields characterize different properties of the reservoir: reflected waves are responsible for its correct positioning in space, while scattered/diffracted waves specify its internal structure. Thus, an adaptive procedure for the construction of seismic wave records is needed for the full description of the reservoir. It should provide for the possibility of constructing images both as regular boundaries, which generate intense reflected waves, and as singular seismogeological objects (points of sharp turns and breaks of boundaries, separate scattering objects and their clusters, and so on), which generate intense scattered waves. It should be noted that the amplitude of regular reflected waves is always significantly higher than that of scattered waves. Therefore, reliable images of singular objects cannot be constructed without the suppression of the regular component of the wave field. Such a procedure of focusing transformation was based on ideas of Yu.A. Tarasov, substantiated, and tested on synthetic and real profiles of the multifold overlap. Its modified version was applied to the study of an areal system of profiles.
机译:1.与经典结构相反,西伯利亚东部的油田通常局限于岩相替代类型的某些局部非均质性。这样的区域通常以高度破裂为特征。因此,它们不仅会产生反射波,还会在地震记录中产生足够强的散射波场。这种区域的地震波场可以表示为反射波和散射/衍射波的叠加。很自然,应该研究两种类型的波场以检查储层结构,因为这两个波场表征了储层的不同特性:反射波负责其在空间中的正确定位,而散射/衍射波则指定了其内部结构。因此,对于储层的完整描述,需要一种用于构造地震波记录的自适应程序。它应提供将图像构造为既可以产生强烈反射波的规则边界,又可以构造成产生强烈反射波的奇异地震地质物体(边界的急转弯和折断点,分离的散射物体及其群等)的可能性。散波。应该注意的是,正反射波的振幅总是明显高于散射波的振幅。因此,如果不抑制波场的规则分量,就无法构建可靠的奇异物体图像。这种集中改造的程序是基于Yu.A. Tarasov,经过证实,并在多重重叠的合成和真实轮廓上进行了测试。它的修改版本被应用于研究剖面系统。

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