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Organic Shale Analysis Using Geochemical Data and Seismic Attributes: Case Study of Talang Akar Formation, South Sumatera Basin

机译:使用地球化学数据和地震属性的有机页岩分析:南苏拉德盆地塔朗·塔尔·塔尔的案例研究

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Organic shale analysis of Talang Akar Formation, south Sumatera basin has been carried out using integrated seismic attributes, petrophysical and geochemical data. This shale layer has been deposited in sagging phase with low deposition energy at transgression period, which results in abundant shale deposit. The paper is aimed at characterizing the geochemical and petrophysical properties of shale rock formation and mapping their distribution using transformed seismic data into acoustic impedance and Total Organic Carbon (TOC). The assessment of this shale formation is carried out by first analyzing rock physics properties to identify the interest zone of a reservoir. The next step is performing geochemical analysis to quantify TOC and determine the maturity level of the shale formation. In order to map the shale formation distribution, we transform seismic data into acoustic impedance and further into organic-rich shale (TOC) distribution. Our analysis of petrophysical and geochemical properties shows that there are two interest zones, in the depth interval of 2030-2182 m (zone A) and 2204-2396 m (zone B). Both zones are predicted as shale layer that has very good organic richness criteria and fulfills sufficient maturity level. In addition, the shale layer distribution is represented by inverted acoustic impedance and TOC, where we found the consistent information related to identified interest zone A and B, which is indicated by relatively low impedance and relatively high TOC. Further, these two zones (zone A and B) are predicted as the potential sweet spot to be explored as unconventional hydrocarbon resource.
机译:南苏米拉盆地的塔朗·塔朗盆地的有机页岩分析已经使用综合地震属性,岩石物理和地球化学数据进行。该页面层已经沉积在脱落相中,在过渡期间沉积能量低,导致岩页沉积物丰富。本文旨在表征页岩岩层的地球化学和岩石物理特性,并使用转化的地震数据将其分布映射到声阻抗和总有机碳(TOC)中。通过首先分析岩石物理性质来识别水库的兴趣区来进行对该页岩形成的评估。下一步正在进行地球化学分析以量化TOC并确定页岩形成的成熟度水平。为了映射页岩形成分布,我们将地震数据转化为声阻抗,进一步进入有机富含物体的页岩(TOC)分布。我们对岩石物理和地球化学特性的分析表明,有两个兴趣区,深度间隔为2030-2182米(A区)和2204-2396M(区域B)。两个区域预测为页岩层,具有非常好的有机丰富标准,并且满足足够的成熟度。另外,页岩层分布由反相声阻抗和TOC表示,在那里我们发现与识别的兴趣区A和B相关的一致信息,其由相对低的阻抗和相对高的TOC表示。此外,这两个区域(区域A和B)被预测为潜在的甜点,作为非传统的烃资源。

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