Driving Tangguh’s First Turbidite Reservoir Development Through New Well Data Integration

A. Prabowo
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Abstract

The Tangguh JV has been producing gas from Bintuni Bay since 2009 from Jurassic Marginal Marine reservoir. The secondary reservoir in Tangguh is the Paleocene Deepwater Turbidite mainly present in Wiriagar Deep (WD) field. This reservoir has been extensively studied but due its complexity and poorer quality compared to the Jurassic, development of this reservoir was not prioritized at first. Poor seismic quality due to karstified overburden made it difficult to image. Evaluation is heavily derived by geology data resulted in robust subregional understanding. The WD Paleocene field consists of four zones, each zone has different Architectural Elements and characteristics including its reservoir quality (Mardani & Butterworth, 2016). It represents classic deepwater turbidite basin evolution, where at the bottom it has deepwater lobes reservoir, then evolves to slope channels overlying it. And lastly covered by shelf and clinoform channel at the top. Slope channel interval is the main development target in the Paleocene reservoir. To inform the best development scenario the subregional understanding needs to be improved. Five development wells targeting Jurassic reservoir closely spaced to each other were drilled in offshore part WD field during 2019-2020. It gave important data for appraising the Paleocene reservoir. Detailed Reservoir Depositional Environment (RDE) map were generated to give guidance in placing the future wells. This RDE map shows where is the on axis, off axis and margin of the slope channel. Integrating subregional understanding with evaluation of this latest data, continued with cellular reservoir model building, and finalized with reservoir simulation, informing the optimum development scenario for the first turbidite reservoir development in Tangguh. Two wells will be drilled in 2022 as part of this program. This development will be a steppingstone to evaluate reservoir performance before expanding the development to onshore and unlock the WD Paleocene field’s full potential.
新井数据整合助力唐古浊积岩储层开发
Tangguh合资公司自2009年以来一直在Bintuni湾开采侏罗纪边际海相储层的天然气。塘古的次生储层为主要分布于Wiriagar Deep (WD)油田的古新世深水浊积岩。该储层已被广泛研究,但由于其复杂性和质量较差,与侏罗纪相比,该储层在一开始并没有得到优先开发。由于覆盖层岩溶,地震质量差,成像困难。评估在很大程度上依赖于地质数据,这些数据导致了对次区域的深入了解。WD古新世油田由四个带组成,每个带都有不同的建筑元素和特征,包括储层质量(Mardani & Butterworth, 2016)。它代表了典型的深水浊积岩盆地演化,其底部为深水叶状储层,然后演化为上覆于其上的斜坡河道。最后被大陆架和斜形水道覆盖。斜坡河道段是古新世储层的主要开发对象。为了为最佳发展设想提供信息,需要增进对分区域的了解。2019-2020年,在海上部分WD油田钻了5口以侏罗系油藏为目标的致密开发井。为古新世储层评价提供了重要资料。生成了详细的储层沉积环境(RDE)图,为后续井的定位提供指导。这张RDE地图显示了斜坡通道的正轴、离轴和边缘。将分区域的理解与最新数据的评价相结合,继续进行单元储层模型的建立,并最终进行储层模拟,为唐古第一个浊积岩储层开发提供了最佳开发方案。作为该计划的一部分,将于2022年钻两口井。在将开发扩展到陆上之前,该开发将成为评估油藏性能的垫脚石,并释放WD古新世油田的全部潜力。
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