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Exploration for gas hydrates in the deepwater,northern Gulf of Mexico:Part I.A seismic approach based on geologic model,inversion,and rock physics principles

机译:墨西哥湾北部深水区天然气水合物的勘探:第一部分:基于地质模型,反演和岩石物理原理的地震方法

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This article presents the results of applying a five-step process for using high-quality seismic data to locate marine gas hydrates.The process involved(1)reprocessing of seismic data for higher resolution,(2)detailed stratigraphic evaluation and interpretation to locate possible hydrate-bearing zones,(3)seismic attribute analysis to further delineate these zones,(4)seismic inversion to obtain appropriate elastic parameters of these zones in 3D,and(5)quantitative estimation of gas hydrate saturation from seismic data using inversion and rock physics principles.We used seismic data from Keathley Canyon 151 and Atwater Valley 14 in the northern Gulf of Mexico.Although careful analysis did indicate the presence of a bottom simulating reflector(BSR),our study mainly relied on a host of other seismic attributes(e.g.,gas chimneys,seismically transparent zones,other features associated with the petroleum system)to characterize the occurrence of gas hydrates in these areas.We tested and verified a viable rock model for hydrate-bearing sediments using data from the Mallik(McKenzie Delta,Canada)and Blake Ridge(ODP Leg 164,southeast U.S.Atlantic margin)wells and modified it for application in the current area.We then used this model to estimate gas hydrate saturation in the host sediments of the northern Gulf of Mexico focus areas using estimates of P-wave and S-wave velocities from inversion of reflection seismic data.In this paper,we present the gas hydrate saturations predicted from the seismic processing methodology prior to 2005 drilling in the focus areas.In frontier areas where no well data are available and lithologic heterogeneities are poorly understood,implementing a seismic-based technique like the one described here to identify potential gas hydrates can provide valuable pre-drill information for site selection and for planning future characterization studies of gas hydrate-bearing sediments.
机译:本文介绍了采用五步过程使用高质量地震数据定位海洋天然气水合物的结果。该过程涉及(1)对地震数据进行再处理以获得更高的分辨率,(2)详细的地层评估和解释以找到可能的位置含水合物带,(3)地震属性分析以进一步界定这些带,(4)地震反演以获得这些带的3D弹性参数,(5)利用反演和岩石从地震数据定量估算天然气水合物饱和度物理原理。我们使用了墨西哥湾北部的Keathley峡谷151和Atwater谷14的地震数据。尽管仔细分析确实表明存在底部模拟反射器(BSR),但我们的研究主要依赖于许多其他地震属性(例如,烟囱,地震透明区域,与石油系统有关的其他特征)来表征这些区域中天然气水合物的发生。我们进行了测试和验证利用Mallik(加拿大麦肯锡三角洲)和Blake Ridge(ODP腿164号,美国东南沿海)的数据,建立了一个可行的含水合物沉积物岩石模型,并对其进行了修改,以用于当前地区。利用反射地震数据反演中的P波和S波速度估算值来估算墨西哥湾北部重点地区宿主沉积物中的天然气水合物饱和度。本文介绍了地震处理过程中预测的天然气水合物饱和度在2005年之前在重点区域进行钻探的方法学。在没有井数据和对岩性非均质性了解不足的边远地区,实施一种基于地震的技术(如此处所述)以识别潜在的天然气水合物可以为钻探提供有价值的信息。选址并计划用于天然气水合物沉积物的未来表征研究。

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