首页> 外文会议>Annual convention of the indonesian petroleum association >POST-MORTEM ANALYSIS OF DRILLING FAILURE OF KAYAN-1 AND KEDUKUL-1 WELLS IN MELAWI BASIN, WEST KALIMANTAN
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POST-MORTEM ANALYSIS OF DRILLING FAILURE OF KAYAN-1 AND KEDUKUL-1 WELLS IN MELAWI BASIN, WEST KALIMANTAN

机译:西红米塔斯西施盆地凯恩-1和KEDUKUL-1井钻机失效后验证分析

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Melawi Basin is one of the basins in Indonesia that has hydrocarbon potential as is indicated by the gas shows encountered by wells and oil seepages at surface. These suggest that the petroleum system in this basin is active. Historically, the basin has attracted some companies to conduct exploration which is marked by the drilling of two wells: Kayan-1 in 1986 and Kedukul-1 in 1995. The drilling reports stated that both wells are dry with gas shows. Therefore, the purpose of this study is to determine the cause of the drilling failure of both wells from a point of view of geological sciences. The research method included analyzing the wells (Kayan-1 and Kedukul-1), seismic data, and research reports to determine the petroleum system in this basin, then by performing further analysis to understand part of the petroleum system components that are not active. Results of the study showed that the potential of the source rock at Kayan-1 and Kedukul-1 is the Ingar Formation. Potential reservoir rocks at Kayan-1 have porosity less than 10% in the upper part of the Ingar Formation and Dangkan Formation. In Kayan-1, the gas shows were observed in the Ingar Formation, Dangkan Formation, and Tebidah Formation. In Kedukul-1. the gas shows were found in the Ingar and Tebidah Fonnations. The Sintang Intrusion occurred in Oligocene - Miocene is found in the several locations and formed some anticlines in Melawi Basin. In Kayan-1 well, the intrusions intruded the Ingar and Dangkan Formations, while in Kedukul-1 the deepest penetrated rocks was the Sintang Intrusion. Conclusion of the study suggests that the drilling failure of Kayan-1 are caused by poor source rock, poor reservoir rock, and the leaking of trap that formed by Sintang intrusion. Drilling failure of Kedukul-1 are caused by the leaking of trap and Sintang intrusion that cause hydrocarbon leaking to the surface.
机译:MELAWI盆地是印度尼西亚的盆地之一,该河水潜力如井在表面上遇到的井和油渗流所示。这些表明该盆地的石油系统是活性的。从历史上看,盆地吸引了一些公司进行探索,这是由两台井的钻井标志的探索:1986年和1995年的Kayan-1和Kedukul-1。钻头报告说,钻头报告说两个孔都有气体表演。因此,本研究的目的是从地质科学的角度来确定两个孔的钻井失败的原因。该研究方法包括分析井(Kayan-1和KeDukul-1),地震数据和研究报告,以确定该盆中的石油系统,然后通过进行进一步的分析来了解未激活的石油系统组件的一部分。该研究的结果表明,Kayan-1和KeDukul-1的源岩的潜力是InGAR形成。凯恩-1的潜在储层岩石在床上形成和埋人的上部孔隙率小于10%。在Kayan-1中,在Ingar形成,Dankan形成和Tebidah形成中观察到气体显示。在Kedukul-1。在ingar和Tebidah Fonnations中发现了气体表演。在几个地点发现寡核苷中发生的Sintang入侵,并在Melawi盆地形成了一些边缘。在凯安-1井中,侵入灌木和南曼的侵入性,而在Kedukul-1中,最深的穿透岩石是Sintang入侵。该研究的结论表明,凯恩-1的钻井衰竭是由源岩,差的储层岩,岩石侵入形成的疏水阀泄漏引起的。 keyukul-1的钻孔失效是由陷阱和内镖侵入引起的,从而导致碳氢化合物泄漏到表面。

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