首页> 外文会议>Annual convention of the indonesian petroleum association >FROM CHAOS TO CAVES - AN EVOLUTION OF SEISMIC KARST INTERPRETATION AT THE VORWATA FIELD
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FROM CHAOS TO CAVES - AN EVOLUTION OF SEISMIC KARST INTERPRETATION AT THE VORWATA FIELD

机译:从混乱到洞穴 - Vorwata领域地震岩溶解释的演变

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Vorwata is a giant gas field located in Bintuni Bay, Papua Barat Province. The Jurassic reservoir has been on production since 2009 with 15 wells drilled from 2 offshore platforms. The overburden in this area is complex and challenging to drill through, especially the thick, karstified carbonate of the Kais and Faumai Formations. These formations have resulted in historical drilling Non-Productive Time (NPT) such as lost circulation, tight hole and stuck pipe. A variety of different seismic surveys have been acquired in this area which includes a large 3D narrow-azimuth towed-streamer survey and a wide-azimuth trenched Ocean Bottom Cable (OBC) survey. The acquired datasets have been reprocessed over time to extract additional value as seismic processing technology evolves. This has provided improvements in subsurface image quality down to the complex carbonate interval. In particular, improvements in the imaging of the Faumai Formation allow more detailed interpretation and have led to an evolution in the understanding of the karst features which range from chaotic to well-defined systems. The 2015 towed-streamer anisotropic Pre-SDM is the latest reprocessing and shows a better image of the karst features compared to the previous towed-streamer isotropic Pre-STM dataset. Further value can be extracted by transforming these new seismic reflectivity volumes to bandlimited impedance. This alternative view of karst features shows a string of low-impedance anomalies which are interpreted as structurally-controlled cave systems instead of tower karst features as previously interpreted on less well focused reflectivity data. These results show some correlation with historical drilling NPT events which make it possible to reduce future occurrences of NPT events for the development wells.
机译:Vorwata是位于宾图尼湾,巴布亚省巴拉一个巨大的气场。自2009年以来侏罗纪储一直生产从2个海上平台钻15周的孔中。的在这方面的负担过重是复杂和具有挑战性的钻通,尤其是厚时,凯斯和Faumai地层的喀斯特碳酸盐。这些编队已导致历史钻探非生产时间(NPT)如堵漏,紧孔和卡钻。各种不同的地震勘测的已在此区,其中包括大3D窄方位角拖缆调查和一个宽方位角沟槽海底电缆(OBC)的调查被获取。所获取的数据集已经被再处理随着时间的推移,以提取另外的值作为地震处理技术的发展。这提供了在地下图像质量改进下降到复杂的碳酸盐间隔。特别是,在形成Faumai的成像改进允许更详细的解释,并导致在的喀斯特特征,其从混沌到明确定义的系统的范围的理解的演进。 2015年拖缆各向异性预SDM是最新的再处理和显示的喀斯特更好的图像特征相比之前的拖缆各向同性预STM数据集。进一步的值可以通过将这些新的地震反射率卷带限阻抗提取。这种替代的喀斯特视图设有显示哪些被解释为喀斯特特征上不那么集中的反射率数据如先前解释的结构上控制的洞穴系统代替塔低阻抗异常的字符串。这些结果表明与历史钻探NPT事件,这使得它可以减少NPT事件为开发井的将来出现一定的相关性。

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