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Integrated Geochemical, Geomechanical and Geological (3G) Study of Lower Baong Shale Formation for Preliminary Shale Gas Prospectivity in the North Sumatra Basin

机译:北苏门答腊盆地初步页岩天然气勘探下仓板较低的地球化学,地质力学和地质(3G)研究

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Abstract The most common fallacy in evaluating shale gas potential in a basin is treated similar to those produced in the United States. In fact, each basin has unique characteristics that influence shale facies type and depositional. Lower Baong shale is responsible for source rock filled up sandstones reservoir in the oil and gas field in the North Sumatra Basin. This study reveals the data and facts from the laboratory, drilling, wireline well logs and seismic through the integrated study of geochemistry, geomechanics and geological synthesis of Lower Baong Formation. An understanding of shale geochemistry, mineralogy and geomechanics is very important to understand how the shale reservoir has the potential to reserve and produce when carried out stimulation. Geochemical laboratory analysis is used to determine the richness, maturity and kerogen type. This information is limited to a certain depth point, so that it is necessary to conduct calibrations in order to estimate the shale productive reservoir interval on a wireline log scale. Limited core data and rock mechanics laboratory analysis represented by mineralogy then also calibrated with brittleness index. Thus, geochemical and geomechanical log model tied to the seismic data, is a very useful tool for formation evaluation and broaden the understanding of shale reservoir facies distribution. Understanding shale facies needed to design fracturing horizontal hole in more detail. This study also classify shale based on organic richness, maturity, type, shale strengthness, shale brittleness and clay content. Shale facies in Lower Baong shale can be divided into 3 facies of sweet spot area. Siliceous calcareous mudstone has high potential for shale gas with 2-3.5% of TOC, II-III of kerogen type, maturity depth from 2300m, 350-425m of sweet spot thickness, 10000- 18000psia of UCS, 3000-4000 psia of Young modulus, 0.18-0.22 of Poisson ratio and associated with foreland basin fill deep. Silty-shaly calcareous mudstone has medium potential for shale gas which is associated with foreland basin fill slope. Silty-shaly dolomitic mudstone is associated with foreland basin fill edge that has high potential for shale. The integrated approach for geochemistry and geomechanics is expected to reduce risk in shale gas exploration.
机译:摘要在评价一个盆地页岩气潜力的最常见的谬误被视为类似于在美国生产。事实上,每个流域都有影响页岩相类型和沉积独有的特色。下Baong页岩负责烃源岩充满了砂岩在北苏门答腊盆地的油气田水库。本研究通过地球化学,地质力学和下Baong形成的地质合成的综合研究揭示了从实验室,钻井,电缆测井,地震数据和事实。页岩地球化学,矿物学和地质力学的理解是非常重要的是了解页岩储层进行时的刺激行为如何储备和生产潜力。地球化学实验室分析来确定的丰富性,成熟性和干酪根类型。该信息被限制在一定的深度点,以便它是必要的,以便估计在电缆测井尺度页岩生产储层间隔进行校准。通过矿物学表示有限的核心数据和岩石力学实验室分析然后也校准,脆性指数。因此,依赖于所述地震数据地球化学和地质力学模型的日志,为地层评价非常有用的工具,拓宽页岩储层相分布的理解。了解页岩相需要设计更详细压裂水平井眼。这项研究也应划分页岩基于有机质丰度,成熟度,类型,页岩strengthness,页岩脆性和粘粒含量。在下Baong页岩页岩相可分为甜蜜点面积的3个相。硅质钙质泥岩具有用于页岩气高电位与TOC的2-3.5%,干酪根型的II-III,从2300米成熟深度,甜蜜点厚度的350-425m,UCS的10000- 18000psia,3000-4000 PSIA杨氏模量的的泊松比0.18-0.22和与前陆盆地填充深相关联。粉质-泥质钙质泥岩具有用于其与前陆盆地填充斜率相关页岩气介质的潜力。粉质,泥质白云岩泥岩与具有页岩高电位前陆盆地填充边缘关联。为地球化学和地质力学的综合方法有望减少在页岩气勘探风险。

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