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SUCCESSFUL IDENTIFICATION OF THIN CARBONATE ON PALEO-BASEMENT HIGH: SPECIAL CASE IN PALEMBANG HIGH, SOUTH SUMATRA BASIN

机译:成功识别古基底高层上的碳酸盐稀薄:南苏门答腊盆地古堡高层的特殊情况

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Oil and gas exploration in the carbonate reservoir in South Sumatra Basin has been carried out intensively during the last 20 years, especially after the Kaji-Semoga Giant Oil Field discovery in 1996. In this area, the carbonate rock overlying the paleo-basement high is generally thin and difficult to identify from conventional seismic data. Most of the carbonates in the Palembang High were developed in carbonate platform depositional settings with a minor possibility of patch reef build-ups. It is almost impossible to interpret the presence of the carbonate in 2-D and 3-D seismic without integrating special geophysical efforts with a regional geological model. There is a large variation in the internal rock heterogeneity of the carbonate rocks, which causes a wide range of rock properties, including that of porosity and permeability. The lateral rock facies changes have increased the degree of uncertainty for exploration. Although these changes could be on a small scale, just within a few meters, they could result in unsuccessful exploration drilling. Another difficulty is that there exists the possibility of absence of carbonate reservoir on top of paleo-basement high. Observation of the seismic character of the basement and carbonate rocks on paleo-basement high is crucial. Carbonate rock has its own specific character, for example, thickening of reflector or decrease in frequency. Another aspect affecting the seismic character is the rock immediately above the carbonate. Density and velocity contrast between both types of rocks have caused significant reflectivity contrast. The carbonate rocks in the Palembang High have much higher velocity compared to the overlying Telisa shale. Seismic gather and attribute analyses are useful in that they lower the reservoir risk component. Gather analysis will increase the ability to ascertain the presence of carbonate and tuning effect, and high frequency enhancement applied to seismic data provides the opportunity to generate better seismic interpretation. Instantaneous frequency is the most suitable method for determining the tuning effect of seismic data. However, all of these methods are limited in their application. The objective of this paper is to share our knowledge on cost-effective exploration methods and on how we can successfully determine thin carbonate reservoir on paleo-basement high, Palembang High, South Sumatra Basin.
机译:在过去的20年中,特别是在1996年发现了Kaji-Semoga巨型油田之后,对南苏门答腊盆地碳酸盐岩储层进行了密集的勘探。在该地区,覆盖于古基底高处的碳酸盐岩为通常较薄,很难从常规地震数据中识别出来。巨港中的大多数碳酸盐都是在碳酸盐台地沉积环境中发育的,补丁斑块堆积的可能性很小。如果不将特殊的地球物理努力与区域地质模型相结合,几乎不可能解释2D和3D地震中碳酸盐的存在。碳酸盐岩内部岩石非均质性变化很大,这导致了广泛的岩石性质,包括孔隙度和渗透率。横向岩相变化增加了勘探的不确定性。尽管这些变化可能很小,只有几米之遥,但它们可能导致勘探钻探失败。另一个困难是,在古基底较高的顶部可能没有碳酸盐岩储层。观测古基底高度上的地下室和碳酸盐岩的地震特征至关重要。碳酸盐岩具有其自身的特征,例如,反射层的增厚或频率的降低。影响地震特性的另一个方面是碳酸盐岩正上方的岩石。两种岩石之间的密度和速度对比引起了明显的反射率对比。与上覆的Telisa页岩相比,巨港的碳酸盐岩具有更高的速度。地震收集和属性分析很有用,因为它们可以降低储层风险成分。聚集分析将增强确定碳酸盐的存在和调谐效果的能力,应用于地震数据的高频增强提供了产生更好的地震解释的机会。瞬时频率是确定地震数据调谐效果的最合适方法。但是,所有这些方法的应用都受到限制。本文的目的是分享我们对具有成本效益的勘探方法的知识,以及如何成功确定苏门答腊盆地南部Palembang High古基底高层的薄碳酸盐岩储层。

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