A Unique Volcanic Jatibarang Reservoir: Facies Characterization and Fracture Calculation

Benyamin Benyamin, P. Pratiwi, F. Indah
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Abstract

Jatibarang structure, situated in Jatibarang low, one of the prolific sub-basin in the northwest Java basin, belongs to PT. Pertamina EP working area. One hundred seventy wells have been drilled, from which there were 56 production wells. Forty production wells were sunk on a volcanic reservoir. Since 1970, volcanic Jatibarang has faced disputed facies concepts, porosities heterogeneity, and permeability system. A fractured reservoir model was proposed. It was due to unique high-performance hydrocarbon in the early years, and then steeply depleted in the early next 3 years, and flat over 20 years. A unique petrophysical method was developed with various explosives and effusive facies. This study proposes a new facies determination concept related to unavailable default petrophysical plots usually used in the clastic-carbonate reservoir. The new concept of formation evaluation attempts to distinguish the fractured vitric tuff reservoir and non-reservoir zone, which is both effusive lava and explosive product. Reservoirs differed from common clastic-carbonate, typically high gamma-ray reservoir due to potassium feldspar composition. The fracture existence is reflected by a sonic overrunning density log aligned with a deep resistivity pattern. The width of the fracture apertures was measured, and spacing intensities were calculated. Finally, fracture permeability was estimated comprehensively to describe reservoir performance. Property models built with only sonic and triple combo have been debatable; however, advanced logging of JTB-211 has proven this accuracy method.
贾提巴郎独特火山岩储层:相表征与裂缝计算
Jatibarang构造位于爪哇盆地西北部高产子盆地之一的Jatibarang低地,属于PT. Pertamina EP工作区。已经钻了170口井,其中56口为生产井。在火山油藏上打了40口生产井。自1970年以来,Jatibarang火山岩的相概念、孔隙度非均质性和渗透率系统一直存在争议。提出了裂缝性储层模型。这主要是由于早期开发出了独特的高性能烃类,随后3年初期急剧枯竭,20多年后趋于平缓。针对不同的炸药和喷涌相,开发了一种独特的岩石物理方法。针对碎屑-碳酸盐岩储层中不可用的默认岩物性地块,提出了一种新的相确定概念。新的储层评价概念试图将裂缝性玻璃质凝灰岩储层与非储层区区分开来,即裂缝性玻璃质凝灰岩储层既为涌出熔岩,也为爆炸产物。由于钾长石的组成,储层不同于普通的碳酸盐岩碎屑储层,具有典型的高伽马射线储层。裂缝的存在可以通过与深部电阻率图相匹配的声波超伸密度测井来反映。测量了裂缝宽度,计算了裂缝间距强度。最后综合估算裂缝渗透率,描述储层动态。仅使用sonic和triple combo构建的属性模型一直存在争议;然而,JTB-211的超前测井证明了这种方法的准确性。
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