首页> 外文会议>Indonesian Petroleum Association Twenty-Eighth Annual Convention Vol.1, Feb 26-28, 2002, Jakarta >SEISMIC INTERPRETATION METHODOLOGY FOR FLUVIAL SANDSTONE RESERVOIRS IN WIDURI FIELD, OFFSHORE SOUTHEAST SUMATRA, INDONESIA
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SEISMIC INTERPRETATION METHODOLOGY FOR FLUVIAL SANDSTONE RESERVOIRS IN WIDURI FIELD, OFFSHORE SOUTHEAST SUMATRA, INDONESIA

机译:印度尼西亚苏门答腊东南海上维杜里油田潮汐砂岩储层的地震解释方法学

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A wide range of seismic interpretation methods are used to detect fluvial sandstone reservoirs in Widuri and neighboring oil fields, offshore Southeast Sumatra. High quality 3D seismic data allow individual reservoirs to be imaged separately, and stratigraphic variations result in certain methods being suited to particular parts of the reservoir succession. Relevant techniques are reviewed in terms of both their general use in seismic interpretation, and specific application to the Widuri reservoir section. Amplitude variations result from changes in acoustic impedance, thin bed thickness and complex interference effects. Seismic two-way time differences are used to detect changes in the stratigraphic thickness of thick beds, lateral velocity variations, and lateral phase changes, which produce locally non-chronostratigraphic reflections. Time-shifted horizon slices, frequency variations and certain attribute ratios highlight subtle waveform variations above or below continuous marker horizons, such as coal seams. Amplitude variation with offset (AVO) is a successful lithology indicator. In the upper reservoirs, amplitude at far offset distinguishes sandstone and carbonaceous mudstone, whereas deeper in the succession complex waveform variations with offset identify sandstone reservoirs closely above or below coal seams. Both range-limited and finite-angle stacks are used for 3-D AVO interpretation. In addition to external reservoir form, structural attri- butes, amplitude variations, coherence and trace shape attributes are used to image internal reservoir architecture. Seismic interpretation methodology in Widuri Field has evolved over the past 10 years, from amplitude and isochrons used in initial field development to phase changes on far-angle stacks and 4D seismic used recently. The period from year 1996 to 2000 shows the effectiveness of these techniques in a late phase of field development. During this time over 150 wells have been drilled, with a success ratio of over 90%.
机译:各种各样的地震解释方法被用来探测维苏里河和苏门答腊东南沿海的邻近油田的河流砂岩储层。高质量的3D地震数据使各个储层分别成像,地层变化导致某些方法适合于储层演替的特定部分。综述了相关技术在地震解释中的一般用途以及在Widuri储层中的具体应用。振幅变化是由声阻抗,薄的床层厚度和复杂的干扰效应引起的。地震双向时差用于检测厚层的地层厚度变化,横向速度变化和横向相位变化,这些变化会产生局部非计时地层反射。时移的层位切片,频率变化和某些属性比突出了连续标记层位(例如煤层)上方或下方的细微波形变化。振幅随偏移的变化(AVO)是成功的岩性指标。在上层储层中,远偏移处的振幅可以区分出砂岩和碳质泥岩,而在具有偏移的连续复杂波形变化的较深处,则可以识别出紧邻煤层上方或下方的砂岩储层。范围限制堆栈和有限角度堆栈均用于3-D AVO解释。除了外部储层形式外,还使用结构属性,幅度变化,相干性和迹线形状属性来对内部储层体系结构进行成像。 Widuri油田的地震解释方法在过去10年中得到了发展,从最初的油田开发中使用的振幅和等时线到远角叠层的相变和最近使用的4D地震。从1996年到2000年这段时期显示了这些技术在油田开发后期的有效性。在此期间,已钻探了150多口井,成功率超过90%。

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