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Identification of Lithology in Gulf of Mexico Miocene Rocks

机译:墨西哥海茂岩岩石岩性识别

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In the Gulf of Mexico, many gas-saturated sands are not Bright Spots and thus are difficult to detect on conventional 31) seismic data. These small amplitude reflections occur frequently in Pliocene-Miocene exploration plays when the acoustic impedances of the gas-saturated sands and shales are approximately the same. In these areas, geophysicists have had limited success using AVO to reduce the exploration risk. The interpretation of the conventional AVO attributes is often difficult and contains questionable relationships to the physical properties of the media. A 3D AVO study was conducted utilizing numerous well-log suites, core analyses, and production histories to help calibrate the seismic response to the petrophysical properties. This study resulted in an extension of the AVO method to a technique that now displays Bright Spots when very clean sands and gas-saturated sands occur. These litho-stratigraphic reflections on the new AVO technique are related to Poisson's ratio, a petrophysical property that is normally mixed with the acoustic impedance on conventional 3D migrated data.
机译:在墨西哥湾,许多气体饱和的砂体不是亮点,因此难以检测常规31)地震数据。当气饱和砂和避沙的声学阻抗大致相同时,这些小幅度反射频繁发生在全茂 - 中间型勘探中。在这些领域,地球物理学家的成功取得有限,以减少勘探风险。传统的AVO属性的解释通常很困难,并且包含与媒体的物理属性的可疑关系。利用众多井 - 日志套件,核心分析和生产历史进行3D AVO研究,以帮助校准对岩石物理性质的地震反应。该研究导致AVO方法的延伸到现在在非常干净的砂和气体饱和的砂体时显示出亮点的技术。这些关于新AVO技术的Litho-stratibraphach的反映与泊松比,通常与传统3D迁移数据上的声阻抗混合的岩石物理。

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