Field X, Central Luconia, Offshore Sarawak, Malaysia, Early Appraisal Stage Reservoir Characterization

K. Poret, A. Saller, P. Henglai, K. Laitrakull, P. Chongrueanglap, W. Siriwattanakajorn, Platt Chris
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Abstract

Miocene carbonates have been producing gas in Central Luconia for more than 30 years (Warrlich et al., 2019). Approximately 65 TCF of recoverable gas have been discovered to date in these build-ups (Scherer, 1980; Mahmud and Saleh, 1999; Khazali et al., 2013; Kosa et al., 2015; Warrlich et al., 2019). One of the most recent carbonate discoveries in this region, Field X, is in its early-stage of reservoir characterization. Depositional and facies models have been created with newly acquired data from LL-C appraisal well. Tectonics, accommodation, and sea level contributed to the overall shape and deposition of the carbonate buildup. One appraisal well, LL-C was drilled and penetrated a thick carbonate section on the structure. With the available data, facies and conceptual depositional models were created using well logs, sidewall cores, conventional cores, cuttings, seismic, and an extensive literature review. At the time of this study, core laboratory analyses were not yet completed. The reservoir is separated into five zones based on well log, core, and seismic data. A precursory facies model was completed using only photographs from the sidewall cores acquired in all five zones of the structure and photographs from conventional core acquired in the upper reservoir interval. Five facies were identified: Coral, Packstone, Wackestone, Mudstone, and Cemented Margin. The data acquired in LL-C illustrates the complexity of carbonate reservoirs and the need to acquire core early in the appraisal of carbonate reservoirs.
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马来西亚海上Sarawak, Central Luconia油田X,早期评价阶段储层表征
中新世碳酸盐已经在中央卢科尼亚生产了30多年的天然气(Warrlich et al., 2019)。迄今为止,在这些堆积中已发现约65万亿立方英尺的可采天然气(Scherer, 1980;Mahmud and Saleh, 1999;Khazali et al., 2013;Kosa et al., 2015;Warrlich et al., 2019)。该地区最近发现的碳酸盐岩之一X油田正处于储层表征的早期阶段。利用LL-C评价井新获得的资料建立了沉积相模型。构造、调节和海平面对碳酸盐堆积的整体形状和沉积有影响。其中一口评价井LL-C在该构造上钻穿了一层较厚的碳酸盐岩剖面。根据现有数据,通过测井、侧壁岩心、常规岩心、岩屑、地震和广泛的文献回顾,建立了相和概念沉积模型。在本研究进行时,核心实验室分析尚未完成。根据测井、岩心和地震数据,将储层划分为五个区域。仅使用在该构造的所有五个区域获得的侧壁岩心照片和在上部储层段获得的常规岩心照片,就完成了前兆相模型。确定了五种相:珊瑚相、包岩相、瓦克岩相、泥岩相和胶结边缘相。LL-C储层获得的数据说明了碳酸盐岩储层的复杂性以及在碳酸盐岩储层评价中早期获取岩心的必要性。
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