张帆2,
王敏3,
唐洪明1,2,
胡钦红4,
张欣吉5
1. 油气藏地质及开发工程国家重点实验室(西南石油大学), 成都 610500
2. 西南石油大学地球科学与技术学院, 成都 610500
3. 中石化胜利油田勘探开发研究院, 山东东营 257015
4. 德克萨斯大学阿灵顿分校地球与环境科学学院, 美国 76019
5. 中国石油新疆油田公司采油二厂, 新疆克拉玛依 834008
基金项目: 国家自然科学基金项目(41830431, 41202110, 51674211), 国家科技重大专项课题(2017ZX05072002), 胜利油田博士后基金项目(YKB1607), 油气藏地质及开发工程国家重点实验室(西南石油大学)开放课题(PLN201809)及四川省科技厅应用基础研究计划项目(2015JY0200)联合资助
详细信息
作者简介: 闫建平, 男, 1980年生, 理学博士, 教授, 主要从事测井地质学、岩石物理及非常规储层测井评价方面的教学与研究工作.E-mail:yanjp_tj@163.com
中图分类号: P631 收稿日期:2018-03-07
修回日期:2018-09-03
上线日期:2019-07-05
Classification of rock-electro parameters of low-permeability sandstone based on nuclear magnetic resonance log and its appication: An example of Es4 in south slope of the Dongying depression
YAN JianPing1,2,,ZHANG Fan2,
WANG Min3,
TANG HongMing1,2,
HU QinHong4,
ZHANG XinJi5
1. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, China
2. School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, China
3. Institute of Exploration and Development, Shengli Oil Field, SINOPEC, Dongying Shandong, 257015, China
4. Department of Earth and Environmental Science, University of Texas at Arlington, Texas 76019, USA
5. No.2 Oil Production Plant, Xinjiang Oilfield Company, PetroChina, Karamay Xinjiang 834008, China
MSC: P631
--> Received Date: 07 March 2018
Revised Date: 03 September 2018
Available Online: 05 July 2019
摘要
摘要:低渗透砂岩储层孔隙结构复杂, 储层有效性识别及饱和度准确计算难度较大.笔者以东营凹陷南坡沙四段(Es4)低渗透砂岩为研究对象, 根据压汞、物性、薄片及核磁等资料, 将研究区孔隙结构分为三大类、五小类.在岩样孔隙结构分类基础上, 明确了孔隙结构类型与岩电参数之间存在确定的关系, 而核磁共振T2谱定量特征参数在一定程度上能够表征孔隙结构类型及其细节信息, 通过提取T2谱中T2几何平均值(T2g)、T2均值(
关键词: 低渗透砂岩/
孔隙结构/
核磁共振T2谱/
岩电参数/
饱和度
Abstract:Comlpex pore structure makes it difficult to identify the reservoir validity and calculate the saturation accurately of low permeability sandstone. This work attempted to address this issue taking the forth member of the Eocene Shahejie Formation (Es4) of the south slope in Dongying Depression as an example. Based on data of mercury injection, physical properties, thin sections and nuclear magnetism, the pore structure of low permeability sandstone in this area was divide into to 3 main types and 5 branch types, which permitted to determine the relationship between pore structure types and rock-electro parameters. Quantitative parameters of NMR T2 spectrum can characterize the pore structure types and its detailed information to some extent. By extracting the parameters of pore structure, such as T2 geometric mean (T2g) and T2 mean (
Key words:Low permeability sandstone/
Pore structure/
T2 spectrum of NMR/
Rock-electro parameters/
Saturation
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