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Diagenesis and porosity evolution of sandstone reservoirs in the East Ⅱ part of Sulige gas field, Ordos Basin

机译:鄂尔多斯盆地苏里格气田东二段砂岩储层成岩作用与孔隙演化

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摘要

It is becoming an important controlling factor of gas exploration and exploitation in the east part of Sulige gas field in the Ordos Basin where the reservoir of main gas formations is tight sandstones.Employing experimental methods of slice identification,casting slice,scan electron microscope,and X-ray diffractions,we studied the characteristics of petrology and diagenesis on reservoirs in Shan1 section of Shanxi formation and He8 section of Shihezi formation of the Permian system in the East Ⅱ part of Sulige gas field.The results include:(1) the main sandstones in these areas are dominated by lithic sandstone and lithic silicarenite with low grade of maturity; (2) the diagenesis of sandstone in these areas mainly include compaction,cementation,corrosion and alteration.Conclusions are as follows:(1) the diagenetic stage reached period B of the middle diagenetic stage; (2) the early diagenetic compaction is one of the main factors to decreasing porosity:(3) the secondary pores formed by corrosion in acidity medium conditions in period A of the middle diagenetic stage can distinctly ameliorate the poor reservoir capability of sandstone and; (4) cementation in period B of the middle diagenetic stage is the most important factor leading to poor physical property of sandstone reservoirs.
机译:它正在成为鄂尔多斯盆地苏里格气田东部气体勘探和剥削的重要控制因素,其中主煤层的储层是紧密的砂岩。施用切片识别,铸造切片,扫描电子显微镜的实验方法和X射线衍射,我们研究了山西山西地层山润的山岩岩石岩层的特点及东Ⅱ部分苏梅田二叠系体系的Shihezi形成的HE8段。结果包括:(1)主要这些区域的砂岩由岩石砂岩和岩石硅石占主导地位,具有低等级的成熟度; (2)这些领域的砂岩的成岩作用主要包括压实,胶结,腐蚀和改变。结论如下:(1)达到中间成岩阶段的成岩阶段B期间B; (2)早期作用压实是降低孔隙率的主要因素之一:(3)中间成岩阶段的酸性介质条件下通过腐蚀形成的二次孔可以明显改善砂岩的较差的储层能力和; (4)中期B期间B期间的胶结是导致砂岩水库差的最重要因素。

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  • 来源
    《矿业科学技术(英文版)》 |2012年第3期|311-316|共6页
  • 作者单位

    Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Geological Sciences and Engineering,Shandong University of Science and Technology, Qingdao 266510, China;

    Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Geological Sciences and Engineering,Shandong University of Science and Technology, Qingdao 266510, China;

    Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Geological Sciences and Engineering,Shandong University of Science and Technology, Qingdao 266510, China;

    Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Geological Sciences and Engineering,Shandong University of Science and Technology, Qingdao 266510, China;

  • 收录信息 中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 chi
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