石油与天然气地质 ›› 2015, Vol. 36 ›› Issue (3): 409-415.doi: 10.11743/ogg20150309

• 层序与储层 • 上一篇    下一篇

伊朗Zagros盆地西南部白垩系Sarvak组碳酸盐岩储层特征

闫建平1,2, 司马立强2, 谭学群3, 张文才3, 梁强2, 言语2   

  1. 1. 西南石油大学 天然气地质四川省重点实验室, 四川 成都 610500;
    2. 西南石油大学 地球科学与技术学院, 四川 成都 610500;
    3. 中国石化 石油勘探开发研究院, 北京 100083
  • 收稿日期:2014-07-11 出版日期:2015-06-08 发布日期:2015-07-24
  • 第一作者简介:闫建平(1980—),男,副教授,测井沉积学、岩石物理及非常规储层测井评价技术。E-mail:yanjp_tj@163.com。
  • 基金项目:
    国家科技重大专项(2011ZX05031-003-006HZ);国家自然科学基金项目(41202110);四川省应用基础研究项目(2015JY0200);胜利油田低渗透示范基地项目(30200000-13-ZC0607-0050);西南石油大学校级科技基金项目(2012XJZ004);四川省教育厅天然气地质创新团队项目(13TD0024)。

Carbonate reservoir characteristics of the Creataceous Sarvak Formation in southwestern Zagros Basin,Iran

Yan Jianping1,2, Sima Liqiang2, Tan Xuequn3, Zhang Wencai3, Liang Qiang2, Yan Yu2   

  1. 1. Sichuan Key Laboratory of Natural Gas Geology, Southwest Petroleum University, Chengdu, Sichuan 610500, China;
    2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China;
    3. Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083, China
  • Received:2014-07-11 Online:2015-06-08 Published:2015-07-24

PDF (PC)

741

被引次数

7

摘要： 为了阐明伊朗Zagros盆地西南部白垩系Sarvak组碳酸盐岩储层特征，利用岩心、薄片、录井、试油及测井资料，通过储层岩性类型、储集空间、物性、电性特征及孔隙发育的影响因素分析，指出Zagros盆地西南部白垩系Sarvak组碳酸盐岩储层岩性类型有白垩质灰岩、云质灰岩、颗粒灰岩，储集空间类型多，主要为次生溶孔、铸模孔，其中颗粒灰岩的物性最好，白垩质灰岩中白垩质主要为浮游有孔虫，孔隙较发育，一般随物性增加，含油性级别升高。成岩作用对储层物性影响也较大，起建设性的成岩作用有溶蚀作用、白云化作用、生物扰动及压溶产生缝合线、缝合面。泥粒灰岩、粒泥灰岩在这些成岩作用的影响下，物性有较大改善。储层孔隙发育微观上主要受控于岩相、成岩作用，平面上还和构造位置及沉积环境有关，位于构造高部位的台地浅滩微相往往物性较好。利用垂向上测井响应及平面上小层物性分布特征，明确了物性较好、含油丰度较高的层段，为寻找高产有利储层提供了依据。

关键词: 低阻, 台地浅滩, 白垩质灰岩, Sarvak组, Zagros盆地

Abstract: In order to reveal the characteristics of the Cretaceous Sarvak Formation carbonate reservoir in the southwestern Zagros Basin, a comprehensive study was carried out by integrating the core, thin section, production test and well log data.Analyses of the reservoir rock types, reservoir space, physical property, electrical property and the factors influencing pore development show that the lithology types of the Sarvak reservoir includes chalky limestone, dolomitic limestone and grainstone.And the reservoir spaces are dominated by secondary dissolved pores and mold pores.The physical property of grainstone is the best.The chalk in chalky limestone is mainly planktonic foraminifera which have well-developed porosity.Generally, the oil-bearing property enhances with the improvement of physical property.The diagenesis also have great impact on reservoir's physical property, and the constructive diagenesis include dissolution, dolomitization, biological disturbance, stylolites of pressolution origin.The physical property of packstone and wackestone are greatly improved under the influences of these constructive diageneses.Microscopically, the development of reservoir's pore is mainly controlled by facies and diagenesis.Laterally, it is also related to tectonic location and sedimentary environment.The physical pro-perty of platform shoal microfacies on structural high is commonly better.The vertical logging response and the areal distribution of physical property of sublayers can be used to identify zones with better physical property and oil-bearing abundance, thus providing a basis for highly productive reservoirs.

Key words: low resistivity, shoal facies, chalky limestone, Sarvak Formation, Zagros Basin

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