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鄂尔多斯盆地马岭地区长8储层成岩作用与有利成岩相带

陈大友 朱玉双 张皎生 杜守礼 桑轼辙 李超 刘萍

陈大友, 朱玉双, 张皎生, 杜守礼, 桑轼辙, 李超, 刘萍. 鄂尔多斯盆地马岭地区长8储层成岩作用与有利成岩相带[J]. 石油实验地质, 2015, 37(6): 721-728. doi: 10.11781/sysydz201506721
引用本文: 陈大友, 朱玉双, 张皎生, 杜守礼, 桑轼辙, 李超, 刘萍. 鄂尔多斯盆地马岭地区长8储层成岩作用与有利成岩相带[J]. 石油实验地质, 2015, 37(6): 721-728. doi: 10.11781/sysydz201506721
Chen Dayou, Zhu Yushuang, Zhang Jiaosheng, Du Shouli, Sang Shizhe, Li Chao, Liu Ping. Diagenesis and favorable diagenetic facies of the eighth member of Yanchang Formation in Maling area, the Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(6): 721-728. doi: 10.11781/sysydz201506721
Citation: Chen Dayou, Zhu Yushuang, Zhang Jiaosheng, Du Shouli, Sang Shizhe, Li Chao, Liu Ping. Diagenesis and favorable diagenetic facies of the eighth member of Yanchang Formation in Maling area, the Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(6): 721-728. doi: 10.11781/sysydz201506721

鄂尔多斯盆地马岭地区长8储层成岩作用与有利成岩相带

doi: 10.11781/sysydz201506721
基金项目: 国家科技重大专项(2008ZX05013-005)和西北大学研究生自主创新项目(YZZ13012)资助。
详细信息
    作者简介:

    陈大友(1987—),男,博士研究生,从事油气田地质与开发研究。E-mail:dychenhn@126.com

  • 中图分类号: TE122.2

Diagenesis and favorable diagenetic facies of the eighth member of Yanchang Formation in Maling area, the Ordos Basin

  • 摘要: 运用常规薄片、铸体薄片、X射线衍射、阴极发光及扫描电镜等实验手段,研究鄂尔多斯盆地马岭地区延长组长8砂岩储集层成岩作用类型及其对储层的影响,划分成岩相并预测有利成岩相带。研究结果表明,研究区长8储层经历了压实、胶结、溶解及交代等多种成岩作用,压实作用和晚期含铁碳酸盐胶结作用使砂岩孔隙大量减少,显著降低储层物性,而溶解作用产生了较多次生孔隙,使储层物性得到明显改善。根据储层物性的主控成岩作用,结合孔隙类型,该区砂岩储集层划分为强溶蚀剩余粒间孔+溶蚀孔相、弱胶结剩余粒间孔相、黏土矿物胶结相、碳酸盐胶结相和强压实相5种成岩相,其中强溶蚀剩余粒间孔+溶蚀孔相和弱胶结剩余粒间孔相储层物性较好,是储层发育的有利成岩相带。

     

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  • 收稿日期:  2015-06-20
  • 修回日期:  2015-10-10
  • 刊出日期:  2015-11-28

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