首页> 外文会议>Annual convention of the indonesian petroleum association >UNLOCKING A CARBONATES RESERVOIR RIDDLE: A POST MORTEM OF THE K-2 APPRAISAL WELL DRY HOLE IN THE SALAWATI BASIN, WEST PAPUA, INDONESIA
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UNLOCKING A CARBONATES RESERVOIR RIDDLE: A POST MORTEM OF THE K-2 APPRAISAL WELL DRY HOLE IN THE SALAWATI BASIN, WEST PAPUA, INDONESIA

机译:解锁碳酸盐储层谜语:在印度尼西亚西巴帕瓦斯萨拉瓦蒂盆地的K-2评估井干洞的后验验

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The Kais carbonate formation has been explored and developed as an oil and gas producing formation in the Salawati basin area since 1939. In 2000, the JOB Pertamina- Santa Fe successfully discovered hydrocarbons in the K structure with the K-1 exploration well, which tested with a result of 900 BOPD with good reservoir properties though several pay zone intervals. In 2013, the JOB Pertamina-Petrochina drilled the K-2 appraisal well in the K structure flank to confirm reserves, and hydrocarbons showed in drill cuttings but well testing results showed a poor accumulation of hydrocarbon. This resulted in many questions that ,. needed to be answered, such as what was the underlying explanation for these results? Also, is the K-l and K-2 reservoir still on the same built up reef body? Is the fault sealing or leaking? Is the hydrocarbon migration enough to full fill the structure? This paper discusses how to answer these questions using a static geological model. To perform the static model, good data was provided after the K-2 well had been drilled. An open hole logging measurement has been taken from the K-2 well, including an advance log such as FMI, dipole sonic and MDT. Also, conventional core has been taken from K-2 well and laboratory analysis has been conducted. The K-l well has a good quality of wire line log and also has a sidewall core taken from several depths including a pay interval. This data was evaluated through a multidiscipline study and concluded with interpretation gathering by building a static model of the K structure. A geological concept has been built using the pattern of the secondary porosity appears. Rock type model has been built by guided of facies model, and following property of reservoir been built by guide of rock type model. Then, the complexity of carbonate can be simplified and successfully show how hydrocarbons accumulated in the K structure and explain the results of the K-2 appraisal well.
机译:已探讨KAIS碳酸盐酯形成,并在1939年以来的Salawati盆地地区的制造形成。2000年,Pertamina-Santa Fe在K-1勘探井中成功发现了K结构中的碳氢化合物,测试了结果有900个Bopd,虽然几个工资区间隔,但仍有良好的水库属性。 2013年,在K结构侧翼钻井作业Pertamina-Petrochina在K结构侧面钻井以确认储备,烃类烃源显示出较差的碳氢化合物累积差。这导致了许多问题,。需要回答,例如这些结果的基本解释是什么?另外,K-L和K-2水库还在同一个内置礁体吗?是故障密封还是泄漏?碳氢化合物迁移是否足以充分填充结构?本文讨论了如何使用静态地质模型回答这些问题。为了执行静态模型,在钻井K-2井之后提供了良好的数据。已经从K-2井中取出了开放孔记录测量,包括预先日志,如FMI,偶极声音和MDT。此外,常规核心已从K-2井中取出,并进行了实验室分析。 K-L井具有良好的线线原木质量,并且还具有从包括付费间隔的几个深度取出的侧壁芯。通过多学科研究评估该数据,并通过构建K结构的静态模型来通过解释采集结束。使用次要孔隙度的模式建立了地质概念。岩型模型是由面部模型的制造构建的,后者通过岩石型模型引导构建了水库的属性。然后,可以简化碳酸盐的复杂性并成功地展示如何在K结构中积聚的碳氢化合物并解释K-2评估的结果。

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