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Reservoir characteristics and favorable area prediction of Devonian Kizirtag formation in Bashituo area, Tarim Basin

机译:塔里木盆地八十tu地区泥盆纪叠统储层特征及有利区域预测

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摘要

Tarim Basin is the largest petroleum potential in the west of China. As a co-prospecting project, some wells of the Devonian Kizirtage formation in Bashituo area have gained encouraging industrial oil flow. The basic characteristics of the reservoir beds are described in detail in this paper by collecting and processing plenty of existing data. The results of petrologic analysis show that the pore types of the Kizirtag formation are mainly residual primary intergranular pores and intergranular dissolution pores, and the lithology is mainly fine grain quartz sandstone. Based on the analyses of reservoir physical properties, the reservoir porosities of Kizirtag formation in study area mainly range from 2% to 8% with an average of 6.14%, and the reservoir has a lower permeability with a range less than 1 × 10~(-3) pm~2 with average of 1.86 × 10~(-3) pm~2. The core analyses indicate there is a distinct positive correlation between porosity and permeability, and members 4 to 6 are the main reservoir section. The inversion prediction of reservoir physical properties shows that the distributions of favorable zones are similar to the distribution of sand body and sedimentary facies. The favorable zones of reservoir physical property of member 6 in Kizirtag formation range from well BK8 to well BK2 and the northern area. Well Q003 and the south eastern area have the poorest physical properties. The favorable zones of reservoir physical property of member 5 distribute in the northwestern and south central area of the study area. The favorable zones of reservoir physical property of member 4 distribute in well BK8 area. Through the statistics analysis, it was found that the reservoir physical properties in study area were controlled by primary sedimentary environment and diagenetic transformation and was especially influenced by the carbonate cementation. There is an obvious negative correlation between the carbonate content and porosity and permeability. Based on the tectonic characteristics, reservoir distributions and hydrocarbon test results of the study area, the favorable areas of main productive layers in the Kizirtag formation were divided to I type, II type and III type. The I type area with the optimum forming conditions is the most favorable part for oil and gas accumulation. So it is suitable to immediately implement drilling, which poses a low drilling risk. The I type areas of the sixth member in the Kizirtag formation is mainly distributed in the intensive areas of exploration wells. The I type areas of the fifth member are mainly concentrated in east in the study area, and the distribution of I type areas in the fourth member of Kizirtag formation is similar to that of the sixth member, but the range is reduced. The distribution of the fourth member is concentrated in the Q002 well to BK9 well range. The II type area has better reservoir forming conditions, and belongs to a more favorable area for hydrocarbon accumulation. However, there are also some exploration risks . In II type areas it is appropriate to carry out drilling to explore objects combined with other hydrocarbon bearing series. The II type areas of the sixth member in Kizirtag formation is concentrated in the east of the study area,; that of the fifth member basically covers the scope of the two traps that are interpreted in this study. In addition, there are larger distribution areas in the east of the study area, and a small distribution area in the south western part of the study area. The II type area distribution of the fourth member in the Kizirtag formation is diminshed, and is mainly distributed in the north of the study area. The reservoir formation conditions of III type zone are poor, so there is no drilling under its current condition. It was considered that this research can provide a new method for future exploration of this area.
机译:塔里木盆地是中国西部最大的石油潜力。作为一项共同勘探项目,位于巴什托地区的泥盆纪Kizirtage地层的某些井获得了令人鼓舞的工业油流。本文通过收集和处理大量现有数据来详细描述储层的基本特征。岩石学分析结果表明,Kizirtag地层的孔隙类型主要为残留的原生粒间孔和粒间溶蚀孔,岩性主要为细粒石英砂岩。根据储层物性分析,研究区基兹塔格形成的储层孔隙度主要在2%〜8%之间,平均为6.14%,储层渗透率较低,范围小于1×10〜( -3)pm〜2,平均为1.86×10〜(-3)pm〜2。岩心分析表明,孔隙度和渗透率之间存在明显的正相关关系,而第4至6段是主要的储层段。储层物性反演预测表明,有利区带的分布与砂体和沉积相的分布相似。 Kizirtag地层中6号段储层物性的有利区域范围为BK8井至BK2井及北部地区。 Q003井和东南部地区的物理性质最差。成员5的储层物性有利区分布在研究区的西北和南部中部地区。成员4的储层物性有利区分布在BK8井区。通过统计分析发现,研究区储层物性受初始沉积环境和成岩作用的控制,尤其受碳酸盐胶结作用的影响。碳酸盐含量与孔隙度和渗透率之间存在明显的负相关。根据研究区的构造特征,储层分布和油气测试结果,将基济塔格组主要生产层的有利区域划分为I型,II型和III型。具有最佳成型条件的I型区域是油气聚集的最有利部分。因此,适合立即实施钻孔,这降低了钻孔风险。 Kizirtag组中第六个成员的I型区域主要分布在勘探井的密集区域。第五成员的I型区域主要集中在研究区的东部,基兹塔格组第四成员中I型区域的分布与第六成员类似,但范围减小了。第四个成员的分布集中在Q002井至BK9井范围内。 II型地区具有较好的成藏条件,属于较有利的油气成藏区。但是,也有一些勘探风险。在II型地区,宜进行钻探以与其他含碳氢化合物轴承系列结合的物体。 Kizirtag组第六成员的II型区域集中在研究区域的东部;第五成员的基本涵盖了本研究中解释的两个陷阱的范围。另外,研究区域的东部有较大的分布区域,研究区域的西南部有较小的分布区域。 Kizirtag组第四成员的II型区域分布减少了,主要分布在研究区域的北部。 Ⅲ型带储层形成条件较差,目前条件下无钻探。有人认为这项研究可以为该领域的未来探索提供一种新的方法。

著录项

  • 来源
    《Energy Exploration & Exploitation》 |2011年第5期|p.575-596|共22页
  • 作者单位

    College of Geosciences and Surveying Engineering, China University of Mining & Technology, Beijing 100083, China;

    College of Geosciences and Surveying Engineering, China University of Mining & Technology, Beijing 100083, China;

    College of Geosciences and Surveying Engineering, China University of Mining & Technology, Beijing 100083, China;

    Exploration and Development Research Institute of Northwestern branch company, SIN OPEC, Xinjiang 830011, China;

    College of Geosciences and Surveying Engineering, China University of Mining & Technology, Beijing 100083, China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    reservoir characteristics; kizirtag formation; devonian; bashituo area; tarim basin;

    机译:储层特征脚印形成;泥盆纪bashituo地区塔里木盆地;

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