首页> 外文会议>International Symposium on Current Progress in Mathematics and Sciences >Shale Gas Characterization Based on Geochemical and Geophysical Analysis: Case Study of Brown Shale, Pematang Formation, Central Sumatra Basin
【24h】

Shale Gas Characterization Based on Geochemical and Geophysical Analysis: Case Study of Brown Shale, Pematang Formation, Central Sumatra Basin

机译:基于地球化学和地球物理分析的页岩气特征:棕色页岩,彭凡塘盆地煎页面案例研究

获取原文

摘要

Geochemical and geophysical analyses of shale gas have been carried out in Brown Shale, Middle Pematang Formation, Central Sumatra Basin. The paper is aimed at delineating the sweet spot distribution of potential shale gas reservoir, which is based on Total Organic Carbon (TOC), Maturity level data, and combined with TOC modeling that refers to Passey and Regression Multi Linear method. We used 4 well data, side wall core and 3D pre-stack seismic data. Our analysis of geochemical properties is based on well log and core data and its distribution are constrained by a framework of 3D seismic data, which is transformed into acoustic impedance. Further, the sweet spot of organic-rich shale is delineated by mapping TOC, which is extracted from inverted acoustic impedance. Our experiment analysis shows that organic materials contained in the formation of Middle Pematang Brown Shale members have TOC range from 0.15 to 2.71 wt.%, which is classified in the quality of poor to very good. In addition, the maturity level of organic material is ranging from 373oC to 432oC, which is indicated by vitrinite reflectance (Ro) of 0.58. In term of kerogen type, this Brown shale formation is categorized as kerogen type of II/ III, which has the potential to generate a mixture of gas/oil on the environment.
机译:苏门答腊盆地中部棕色页岩,中部彭港,棕色页岩,中部的地球化学和地球物理分析。本文旨在描绘潜在的页岩气体储层的甜点分布,该储层气体储层基于总有机碳(TOC),成熟程度数据,以及与TOC建模相结合,指的是PASSEY和回归多线性方法。我们使用了4个井数据,侧壁核心和3D堆叠地震数据。我们对地球化学特性的分析基于井数,核心数据,其分布受到3D地震数据的框架的约束,该框架被转变为声阻抗。此外,通过绘制TOC来描绘有机富含物质的甜点,其从倒置声阻抗中提取。我们的实验分析表明,中坪棕色页岩成员形成的有机材料从0.15〜2.71重量%的TOC均为0.15至2.71重量%。%,其归类为穷人的质量。此外,有机材料的成熟水平范围为37.3℃至432oC,其通过0.58的vitriinite反射率(RO)表示。在Kerogen型中,这种棕色页岩形成被分类为Kerogen型II / III,这具有可能在环境中产生气体/油的混合物。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号