首页> 外文会议>Proceedings of The 39th IPA convention and exhibition-Working together to accelerate solutions in anticipating indonesia's energy crisis >EVOLUTION AND KARSTIFICATION OF THE EOCENE-MIOCENE CARBONATES OVERLYING THE TANGGUH GAS FIELDS IN WESTERN PAPUA - OBSERVATIONS FROM 3D SEISMIC AND IMPACT ON DRILLING OPERATIONS
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EVOLUTION AND KARSTIFICATION OF THE EOCENE-MIOCENE CARBONATES OVERLYING THE TANGGUH GAS FIELDS IN WESTERN PAPUA - OBSERVATIONS FROM 3D SEISMIC AND IMPACT ON DRILLING OPERATIONS

机译:西巴布亚塘沽气田上始新世-中新世碳酸盐岩的演化和岩溶化-从3D地震观测及对钻井作业的影响

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The Tangguh gas fields in the Birdshead region of West Papua comprise the giant Vorwata field (currently producing gas to supply two 3.8 MTPA LNG trains) plus three undeveloped smaller structures. The traps have a structural and stratigraphic component, with shallow-marine Jurassic and deep-marine Paleocene clastic reservoirs sourced from deeply buried Jurassic and older shales. Overlying the fields is a complex overburden which presents significant drilling challenges, including the presence of shallow gas, overpressured sands, faults and karst features which lead to losses and hole-instability. Many of these drilling NPT (Non Productive Time) issues are related to drilling through a thick (3000 ft) carbonate sequence of Eocene to Miocene age, locally called the Faumai and Kais sequences.rnThe bulk of the Tangguh area is covered by 3D seismic of a variety of vintages and acquisition techniques, including towed-streamer, land, transition zone and OBC. Modern wide-azimuth OBC seismic is designed for reservoir imaging, while the more laterally-extensive narrow-azimuth towed-streamer dataset (acquired in 1997, and reprocessed several times) gives high-quality images of the overburden down to the carbonate intervals. Coherency and spectral decomposition techniques reveal startling karst features with a variety of geometries and dimensions at a number of key sequence boundaries. Often these seem to be structurally controlled, i.e. following the fabric of the strike-slip influenced faulting that occurred during the protracted and complicated collision between the Australian and the Pacific Plates in the early Tertiary.rnThe evolution and deformation of the Faumai and Kais has been investigated, with evidence for multiple episodes of exposure and karstification punctuating periods of carbonate production. Structural history and original carbonate facies strongly controls the karst development, and can be linked to past drilling problems.
机译:西巴布亚Birdshead地区的Tangguh气田包括巨大的Vorwata气田(目前正在生产天然气,以提供两辆3.8 MTPA液化天然气列车)和三个未开发的较小结构。圈闭具有结构和地层成分,浅海侏罗纪和深海古新世碎屑岩储层来自深埋的侏罗纪和较旧的页岩。气田上空是一个复杂的覆盖层,面临着巨大的钻井挑战,包括浅层气,超压砂,断层和喀斯特地貌的存在,导致损失和井眼不稳定。这些钻探中的许多NPT(非生产时间)问题都与在始新世至中新世的一段厚(3000 ft)碳酸盐岩层序中进行钻探有关,当地称为Faumai和Kais序列。多种年份和采集技术,包括拖缆,土地,过渡带和OBC。现代的宽方位OBC地震是为储层成像而设计的,而横向扩展较窄的拖曳拖缆数据集(于1997年获得,并经过多次处理)给出了覆盖层直至碳酸盐岩层段的高质量图像。相干和频谱分解技术揭示了在多个关键序列边界处具有各种几何形状和尺寸的惊人喀斯特特征。通常这些似乎是结构上受控的,即在第三纪早期澳大利亚和太平洋板块之间长期而复杂的碰撞中发生了走滑影响的断层结构。rnFaumai和Kais的演化和变形已经发生。进行了调查,并发现了碳酸盐生产的多次暴露和岩溶作用标点时期。构造历史和原始碳酸盐相强烈地控制了岩溶发育,并且可能与过去的钻井问题有关。

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