波斯湾西部某油田振幅变化的偏移反演分析

B. Khadem, A. Javaherian
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引用次数: 0

摘要

储层表征在储层地球物理和储层管理中具有主导作用。由于储层地球物理学和储层管理的兴趣在于地下岩石的弹性性质和储层性质,因此需要一种强大的方法将地震数据转换为弹性性质。因此,通过采用岩石物理模型和利用反演地震数据,可以对储层进行描述,以提高储层的产量。在本研究中,我们采用了一种将地震资料转换成弹性性质的方法。这种反演方法被称为同步反演,它被归为振幅随偏移量变化(AVO)反演类别。该方法与其他AVO反演方法不同,将叠前地震资料直接反演为岩石的弹性性质,提供了良好的岩性和流体指标(VP/VS)。然后,在波斯湾的一个油田对该指标进行了测试。此外,利用该方法可以确定流体接触面和岩性夹层的位置;此外,通过反演结果,即岩石地震性质的立方体,可以生成岩石弹性性质的剖面,如泊松比和杨氏模量,这对地质力学分析很有用。因此,这种方法为研究区域的前期分析提供了一种快速的方法。
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Amplitude Variation with Offset Inversion Analysis in One of the Western Oilfields of the Persian Gulf
Reservoir characterization has a leading role in the reservoir geophysics and reservoir management. Since the interests of the reservoir geophysics and reservoir managements are the elastic properties and reservoir properties of the subsurface rock for their purposes, a robust method is required for converting seismic data into elastic properties. Accordingly, by employing a rock physics model and using the inverted seismic data, one can describe the reservoir for purposes such as improvement in the production of the reservoir. In the present study, we employ one of the methods for converting the seismic data into the elastic properties. This method of inversion is known as simultaneous inversion, which is grouped in amplitude-variation-with-offset (AVO) inversion category. In this method, unlike the other methods of AVO inversion, the pre-stack seismic data are directly inverted into the elastic properties of the rock and an excellent lithology and fluid indicator (VP/VS) are provided. Then, this indicator is tested on one of the oilfields of the Persian Gulf. Moreover, by means of this method, one can locate the fluids contact and the lithological interlayers; also, by the inversion results, which are the cubes of the seismic properties of the rock, one can generate sections of the elastic properties of the rock such as Poisson’s ratio and Young modulus which are useful for geomechanical analysis. Therefore, this kind of method is a quick way for the prior analysis of the studied area.
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