油气勘探

鄂尔多斯盆地致密气储集层孔隙流体地震预测方法

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  • 1. 中国石油天然气集团公司,北京 100007;
    2. 低渗透油气田勘探开发国家工程实验室,西安 710018;
    3. 中国石油长庆油田公司勘探开发研究院,西安 710018;
    4. 成都理工大学,成都 610059
杨华(1963-),男,山东菏泽人,博士,中国石油天然气集团公司教授级高级工程师,主要从事石油地质综合研究及油气勘探开发管理工作。地址:北京市东城区东直门北大街9号,中国石油天然气集团公司,邮政编码:100007。E-mail:yang-hua@cnpc.com.cn 联系作者简介:王大兴(1963-),男,甘肃武威人,博士,中国石油长庆油田公司教授级高级工程师,主要从事石油地球物理方法研究和地震储集层预测工作。地址:陕西省西安市未央区长庆兴隆园小区,长庆油田公司勘探开发研究院,邮政编码:710018。E-mail:wdx1_cq@petrochina.com.cn

修回日期: 2016-04-08

  网络出版日期: 2017-07-27

Seismic prediction method of pore fluid in tight gas reservoirs, Ordos Basin, NW China

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  • 1. China National Petroleum Corporation, Beijing 100007, China;
    2. National Engineering Laboratory for Exploration and Development of Low-Permeability Oil & Gas Fields, Xi’an 710018, China;
    3. Exploration and Development Research Institute of PetroChina Changqing Oilfield Company, Xi’an 710018, China;
    4. Chengdu University of Technology, Chengdu 610059, China

Revised date: 2016-04-08

  Online published: 2017-07-27

Supported by

国家自然科学基金项目“非常规油气勘探与开发地球物理基础理论与方法研究”(41390451); 国家科技重大专项“鄂尔多斯盆地大型低渗透岩性地层油气藏开发示范工程”(2016ZX05050)

摘要

基于鄂尔多斯盆地上古生界二叠系下石盒子组盒8段致密储集层岩石物理分析结果,考虑体积模量对孔隙流体敏感的特点,提出了致密储集层岩相控制下利用压缩系数检测流体性质的方法。该方法首先是进行岩相识别,利用叠前反演的纵横波交会技术计算致密砂岩相的分布;其次是在岩相控制下(排除泥质含量影响),利用可稳定反演的波阻抗和速度计算压缩系数;最后利用气水层压缩系数的差异进行储集层孔隙流体性质判识。苏里格致密气田勘探开发生产实践表明:应用压缩系数进行孔隙流体性质识别的效果较好,能有效预测气水层的分布。图9表2参19

本文引用格式

杨华, 王大兴, 张盟勃, 王永刚, 刘力辉, 张盟黎 . 鄂尔多斯盆地致密气储集层孔隙流体地震预测方法[J]. 石油勘探与开发, 2017 , 44(4) : 513 -520 . DOI: 10.11698/PED.2017.04.04

Abstract

Based on the rock physical analysis of tight gas reservoirs in He8 Member of Permian Lower Shihezi Formation of Ordos Basin, and considering that bulk modulus is sensitive to pore fluid, this study proposes a fluid property detection method by compression coefficient of tight sandstone reservoirs under the constraint of reservoir lithofacies. In this method, lithofacies is identified first by calculating distribution of tight sandstone facies with the cross plot of Vp and Vs obtained from pre-stack seismic inversion; secondly, the compression coefficient is calculated by P-wave impendance and velocity from stable pre-stack seismic inversion with the restriction of lithofacies (excluding the influence of clay content); and finally, pore fluid properties are determined using the differences of compression coefficients in gas and water layers. Its application in tight gas exploration and development in Sulige gas field of Ordos Basin shows that this pore fluid prediction method by calculating compression coefficient can effectively and efficiently delineate the distribution of gas-bearing and water-bearing sandstone.

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