首页> 外文会议>Indonesian Petroleum Association Annual Convention >THE IMPACT OF DIFFERENTIAL SUBSIDENCE RATES IN SHALLOW WATER CARBONATE RESERVOIR QUALITY: AN EXAMPLE FROM THE EAST JAVA BASIN, INDONESIA
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THE IMPACT OF DIFFERENTIAL SUBSIDENCE RATES IN SHALLOW WATER CARBONATE RESERVOIR QUALITY: AN EXAMPLE FROM THE EAST JAVA BASIN, INDONESIA

机译:浅水碳酸盐储层质量下​​微分沉降速率的影响:印度尼西亚东爪哇盆地的一个例子

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In Indonesia and much of SE Asia, some of the largest and most prolific hydrocarbon reservoirs are derived from isolated, shallow-water Tertiary carbonate buildups, including Natuna, the fields of north Sumatra, and those of the Cepu block, East Java Basin. ExxonMobil has been exploring and developing gas and oil fields at Cepu since 1999 with the discoveries of Sukowati, Banyu Urip, Cendana and Jambaran fields. The depositional history and controls on carbonate growth of the Cepu block has been of great interest to industry and academia due to the importance of the carbonate buildup play in SE Asia. Reservoir quality in the Cepu fields appears to change with stratigraphic age with the Miocene having better reservoir quality than the Oligocene. In addition, there are reservoir quality differences between fields of similar age. Core analysis and thin section studies show that these isolated carbonate buildups were all deposited as grain dominated shallow water platforms with similar facies distribution. However, there appears to be variation in the amount of diagenetic leaching that controls reservoir quality. Reservoir quality can be correlated directly to subsidence rates. Subsidence rates control the amount of time the fresh water lens has to leach the carbonates and enhance the reservoir quality.
机译:在印度尼西亚和SE亚洲的大部分地区,一些最大和最多的碳氢化合物储层源自孤立,浅水三级碳酸盐底座,包括Natuna,North Sumatra的领域以及East Java Basin的Cepu Block的领域。自1999年以来,埃克森美孚一直在探索和开发CEPU的天然气和油田,并发现Sukowati,Banyu Urip,Cendana和Jambaran领域的发现。由于SE亚洲碳酸盐堆积在亚洲碳酸盐累积的重要性,CEPU Block对CEPU Block的碳酸酯生长的沉积历史和对照对工业和学术界具有很大的兴趣。 Cepu领域的储层质量似乎随着地层年龄的变化,其中内科具有比少茂更好的水库质量。此外,在类似年龄的领域之间存在储层质量差异。核心分析和薄剖面研究表明,这些分离的碳酸盐堆积全部沉积为具有相似相分布的晶粒占浅水平台。然而,控制储层质量的成岩浸出量似乎是变化的。水库质量可以直接与沉降速率相关联。沉降速率控制淡水透镜必须浸出碳酸盐并提高储层质量的时间。

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