茉莉田,泰国湾,断层充填和泄漏历史:断层密封校准

R. Davies, P. Wilson, D. Povey, Pattarapong Prasongtham, Siriporn Shibano, T. Ampaiwan, Farid Saifuddin
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引用次数: 0

摘要

在作业油田中,储层的分区化通常是由断层的封闭引起的(cery等,2004;Davies and Handschy, 2003;Davies et al., 2019;Knipe, 1992;yield et al., 1997;yield et al., 2010)。然而,如果没有足够的地下数据,就很难校准这种密封。本研究选择了位于泰国湾Pattani盆地北部的Jasmine油田中部的一个局部区域Jasmine A进行详细的断层封闭分析校准。目的是通过对断层的并置分析来呈现填充和溢出历史的细节。大量具有流体和岩相数据的井眼以及渗透率分布的三维模型提供了一个地下框架,以减少不确定性,并允许对断层间储层并置和流体接触水平进行更全面的分析。通过检查断层走向视图中的流体接触,并将其性质并置,评估了断层间的流动行为和充填和溢出历史。茉莉花田是一个狭窄的构造隆起,由许多NE-SW和NNW-NNE走向的断裂切割而成,形成断界分隔室。该油田的储层为典型的薄层高渗透率河流砂岩,主要为中新世,由数千米深的薄页岩层隔开。许多砂岩具有独特的油气和水的接触面。断层上的储层并置表明断层封闭性在圈闭中起主要作用。通过比较每个断块中的流体接触,在断层上具有不同接触的情况可能代表断层膜密封。接触发生在同一高度表明跨断层漏电。通过估算断层的渗透率分布来进行评价。然而,这些结果并不能仅仅从断层两侧的流体接触中充分确定:邻近断块的充填历史和侧向构造控制也必须考虑在内。这些结果结合在一起,可以定义一个独特的填充和溢出历史。对茉莉花A地区局部构造圈闭的主要断层并置分析结果为断层的三维分析提供了校准,包括断层岩石性质的估计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Jasmine Field, Gulf of Thailand, Fill and Spill History Across Faults: A Fault-Seal Calibration
Compartmentalization of reservoirs in operating fields is commonly caused by sealing of faults (Cerveny et al., 2004; Davies and Handschy, 2003;Davies et al., 2019; Knipe, 1992; Yielding et al., 1997; Yielding et al., 2010). Calibrating this seal, however, is difficult without adequate subsurface data. A local region across the central part of the Jasmine Field, Jasmine A, along the northern extent of the Pattani basin in the Gulf of Thailand, was selected in this study for detailed fault-seal analysis calibration. The objective was to present the details of the fill and spill history from a juxtaposition analysis across the faults. The large number of well penetrations with fluid and lithofacies data and the 3D models of mapped permeability distribution provided a subsurface framework to reduce the uncertainty and allow a more comprehensive analysis of the crossfault reservoir juxtaposition and fluid contact levels. Crossfault flow behavior and fill and spill history were evaluated by examining fluid contacts in a strike view of the fault, with the properties juxtaposed. The Jasmine Field is a narrow structural high that is cut by many NE-SW and NNW-NNE trending faults forming fault-bounded compartments. Reservoirs in the field are typically thin, stacked high-permeability fluvial sandstones of primarily Miocene age separated by thin shale beds that occur over a depth range of several thousand meters. Many of the sands have unique hydrocarbon-water contacts of oil or gas and water. Reservoir juxtaposition across the faults suggests that fault seal plays a major role in the trap. By comparing fluid contacts in each fault block, cases with different contacts across the fault likely represent a fault membrane seal. Contacts occurring at the same height suggest crossfault leakage. The evaluation was done by estimating permeability distributions across the fault. These results, however, were not adequately determined simply from the fluid contacts on either side of the fault: fill histories in adjacent fault blocks and lateral structural controls also had to be accounted for. The results together allowed a unique fill and spill history to be defined. The results of the juxtaposition analysis for the main faults bounding the local structural trap in Jasmine A provided a calibration for a 3D analysis of the faults, including estimation of fault-rock properties.
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