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塔里木盆地志留系碎屑岩孔隙成因类型定量分析——以顺9井柯坪塔格组为例

张永东 王恕一

张永东, 王恕一. 塔里木盆地志留系碎屑岩孔隙成因类型定量分析——以顺9井柯坪塔格组为例[J]. 石油实验地质, 2016, 38(3): 413-417. doi: 10.11781/sysydz201603413
引用本文: 张永东, 王恕一. 塔里木盆地志留系碎屑岩孔隙成因类型定量分析——以顺9井柯坪塔格组为例[J]. 石油实验地质, 2016, 38(3): 413-417. doi: 10.11781/sysydz201603413
Zhang Yongdong, Wang Shuyi. Quantitative analysis of pore genetic types in the Silurian clastic rocks in the Tarim Basin: A case study of the Kepingtage Formation in well Shun9[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(3): 413-417. doi: 10.11781/sysydz201603413
Citation: Zhang Yongdong, Wang Shuyi. Quantitative analysis of pore genetic types in the Silurian clastic rocks in the Tarim Basin: A case study of the Kepingtage Formation in well Shun9[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(3): 413-417. doi: 10.11781/sysydz201603413

塔里木盆地志留系碎屑岩孔隙成因类型定量分析——以顺9井柯坪塔格组为例

doi: 10.11781/sysydz201603413
基金项目: 中国石化科技部项目"塔里木志留系油气富集主控因素及勘探方向"(P12003)资助。
详细信息
    作者简介:

    张永东(1982-),男,工程师,从事碎屑岩沉积储层和成岩作用研究。E-mail:gentleman10001@163.com。

  • 中图分类号: TE122.2

Quantitative analysis of pore genetic types in the Silurian clastic rocks in the Tarim Basin: A case study of the Kepingtage Formation in well Shun9

  • 摘要: 碎屑岩储层孔隙主要成因类型鉴别,影响到进一步勘探时对储层预测方向的判断。塔里木盆地志留系储层大多为原生-次生复合孔和微孔,仅仅根据铸体薄片观察统计往往难以正确鉴别其主要孔隙成因类型。以顺9井志留系储层为例,在铸体薄片观察统计的基础上,根据相似岩性在相似埋藏条件下,原生孔隙受压实衰减程度相近,其残余原生孔含量相近的原理,综合分析埋深相近层段储层岩石学特征和实测孔隙度,定量化分析该储层段不同成因类型孔隙的含量。统计表明,顺9井志留系储层中原生残余粒间孔含量小于4.6%(实测孔隙度3.2%~14.6%);现今发育的中-低孔储层,主要是叠加了次生溶蚀孔形成的,孔隙度相对较高的储层以次生孔为主。该定量化分析方法可正确判别储层孔隙类型。

     

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出版历程
  • 收稿日期:  2015-05-29
  • 修回日期:  2016-03-22
  • 刊出日期:  2016-05-28

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