吉林大学学报(地球科学版)

• 地质与资源 • 上一篇    下一篇

东营凹陷民丰洼陷北带沙四下亚段深层天然气储层成岩作用

王淑萍1,徐守余1,董春梅1,王丽萍2,刘春平3   

  1. 1.中国石油大学(华东)地球科学与技术学院,山东 青岛266580;
    2.中石化胜利油田东胜集团股份公司,山东 东营257000;
    3. 中石化胜利油田河口采油厂,山东 东营257000
  • 收稿日期:2014-05-08 出版日期:2014-11-26 发布日期:2014-11-26
  • 基金资助:

    国家科技重大专项(2011ZX05009-003)

Diagenesis Characteristics of Deep Natural Gas Reservoirs in Es4x in the North Zone of Minfeng Sag in Dongying Depression

Wang Shuping1,Xu Shouyu1,Dong Chunmei1,Wang Liping2,Liu Chunping3   

  1. 1.School of Geosciences , China University of Petroleum, Qingdao266580,Shandong,China;
    2.Dongsheng Group Co., Ltd of Shengli Oil Field,Sinopec,Dongying257000,Shandong,China;
    3.Hekou Oil Production Plant of Shengli Oil Field  Sinopec ,Dongying257000,Shandong ,China
  • Received:2014-05-08 Online:2014-11-26 Published:2014-11-26
  • About author:王淑萍(1978-),女,博士研究生,主要从事油气储层评价方面研究,E-mail:wshpwyzh0619@163.com

摘要:

由于对东营凹陷民丰洼陷北带深层天然气储层成岩作用特征及其对储层的控制作用认识不清,给该地区天然气勘探带来了极大的风险。综合运用铸体薄片、扫描电镜观察、流体包裹体分析及岩心物性分析等多种技术方法,对东营凹陷民丰洼陷北带沙四下亚段深层天然气储层成岩作用特征及其对储层物性的影响进行了系统的研究。结果表明,该区北带沙四下亚段深层天然气储层为近岸水下扇砂砾岩,成岩作用具有强压实、欠压实、多期溶解、多期胶结、复杂交代和灰泥组分重结晶的特征。主要胶结-溶解作用序列为长石溶解/石英次生加大→碳酸盐胶结/石英溶解→碳酸盐胶结物溶解/石英次生加大→黄铁矿胶结/沥青充填。近岸水下扇不同亚相(微相)沉积特征的差异性导致了埋藏过程中成岩作用的差异性,并决定了储集物性的差异性。扇根砾岩在埋藏过程中成岩作用以压实作用和灰泥杂基重结晶作用为主,溶解作用微弱,物性持续降低。在中深层灰泥杂基的重结晶作用使扇根砾岩物性快速降低而形成致密层,扇根砾岩全部为干层。由于早期异常高压和早期油气充注对储层保护以及酸性溶解对储层改造的综合作用,扇中辫状水道远离泥岩、砂砾岩储层在中深层仍发育大量原生孔隙和少量的次生孔隙,储层物性较好,可作为良好的天然气储层。扇中辫状水道靠近泥岩层储层、扇中水道间以及扇缘部位因发生强烈胶结作用,在砂体顶底形成致密的胶结壳,可作为较好的盖层。

关键词: 成岩作用, 天然气储层, 沙四下亚段, 砂砾岩体, 东营凹陷, 致密砂岩

Abstract:

The diagenetic characteristics of deep natural gas reservoirs and the control of diagenesis on reservoirs in the lower part of the Fourth Member of the Shahejie Formation (Es4x) in the north zone of the Minfeng sag in the Dongying depression haven’t been clearly understood, which have led to great risks to hydrocarbon exploration in this area. Based on a combination of thin-section identification, scanning electron microscope (SEM) observation, fluid inclusion analysis and an analysis of core properties, it has been systematically studied about the diagenetic characteristics and its influence on the reservoir property. Nearshore subaqueous fan glutenite is the main regional reservoirs, and the diagenesis is characterized by strong compaction, poor compaction, dissolution and cementation of many stages, complex metasomatism and lime-mud matrix recrystallization. The main cementation-dissolution sequence is feldspar dissolution/quartz overgrowth →carbonate cementation / quartz dissolution →carbonate dissolution /quartz overgrowth →pyrite cementation and bitumen filling. The difference of sedimentary characteristics in different sub/micro-facies of nearshore subaqueous fan controls the difference of diagenetic characteristics, which also determines the difference of reservoir physical property. The conglomerate in inner fan mainly experiences compaction and lime-mud matrix recrystallization, with weak dissolution, and its physical properties keep reducing. The lime-mud matrix recrystallization results in a rapid reduction of physical properties in middle-deep layers. The present physical property of inner fan becomes extremely poor and mainly develops dry layers. Because acid dissolution reconstruct the reservoirs and early hydrocarbon filling and abnormal high pressure can protect reservoirs, the reservoirs far away from mudstone layers in the braided channels of middle fan develop a great number of primary pores and a few secondary pores, have a higher porosity and permeability, and can be effective reservoirs for natural gas. The parts in interdistributaries of middle fan and outer fan develop intensively cementation, it forms dense cemented crusts at the top of the sandstone, and therefore they mainly act as cap rocks.

Key words: diagenesis, natural gas reservoirs, the lower part of the Fourth Member of the Shahejie Formation of the Paleogene;, glutenite bodies, Dongying depression, tight sandstone

中图分类号: 

  • P618.13
[1] 王玉霞, 周立发, 焦尊生, 尚庆华, 黄生旺. 鄂尔多斯盆地陕北地区延长组致密砂岩储层敏感性评价[J]. 吉林大学学报(地球科学版), 2018, 48(4): 981-990.
[2] 林敉若, 操应长, 葸克来, 王健, 陈洪, 吴俊军. 阜康凹陷东部斜坡带二叠系储层特征及控制因素[J]. 吉林大学学报(地球科学版), 2018, 48(4): 991-1007.
[3] 贾艳聪, 操应长, 林畅松, 王健. 东营凹陷博兴洼陷沙四上亚段滩坝优质储层形成机理与分布特征[J]. 吉林大学学报(地球科学版), 2018, 48(3): 652-664.
[4] 孙海涛, 钟大康, 李勇, 毛亚昆, 杨宪彰. 超深低孔特低渗砂岩储层的孔隙成因及控制因素——以库车坳陷克深地区巴什基奇克组为例[J]. 吉林大学学报(地球科学版), 2018, 48(3): 693-704.
[5] 林承焰, 王杨, 杨山, 任丽华, 由春梅, 吴松涛, 吴玉其, 张依旻. 基于CT的数字岩心三维建模[J]. 吉林大学学报(地球科学版), 2018, 48(1): 307-317.
[6] 蔡来星, 卢双舫, 张训华, 肖国林, 吴志强, 黄文彪. 基于孔喉结构建立致密砂岩储层评价方案——以松南中央坳陷泉四段为例[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1654-1667.
[7] 张焕旭, 陈世加, 路俊刚, 刘超威, 陈娟, 李勇, 徐坤. “膨胀力”作用下致密砂岩储层石油运聚特征[J]. 吉林大学学报(地球科学版), 2017, 47(5): 1341-1351.
[8] 刘鑫金, 冯阵东, 李聪, 周艳, 王亚明. 近源湖盆砂砾岩储层次生溶孔成因探讨——以查干凹陷祥6井区为例[J]. 吉林大学学报(地球科学版), 2017, 47(2): 393-404.
[9] 陈冬霞, 庞雄奇, 杨克明, 祝渭平, 严青霞. 川西坳陷深层叠复连续型致密砂岩气藏成因及形成过程[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1611-1623.
[10] 贾珍臻, 林承焰, 任丽华, 董春梅, 宫宝. 苏德尔特油田低渗透凝灰质砂岩成岩作用及储层质量差异性演化[J]. 吉林大学学报(地球科学版), 2016, 46(6): 1624-1636.
[11] 朱传华, 王伟锋, 王青振, 李玉坤. 非均质储层三维构造应力场模拟方法[J]. 吉林大学学报(地球科学版), 2016, 46(5): 1580-1588.
[12] 刘鹏, 王伟锋, 孟蕾, 姜帅. 鄂尔多斯盆地上古生界煤层气与致密气联合优选区评价[J]. 吉林大学学报(地球科学版), 2016, 46(3): 692-701.
[13] 潘保芝, 蒋必辞, 刘文斌, 房春慧, 张瑞. 致密砂岩储层含气测井特征及定量评价[J]. 吉林大学学报(地球科学版), 2016, 46(3): 930-937.
[14] 李易霖, 张云峰, 丛琳, 谢舟, 闫明, 田肖雄. X-CT扫描成像技术在致密砂岩微观孔隙结构表征中的应用——以大安油田扶余油层为例[J]. 吉林大学学报(地球科学版), 2016, 46(2): 379-387.
[15] 陈波, 王子天, 康莉, 张顺存, 史基安. 准噶尔盆地玛北地区三叠系百口泉组储层成岩作用及孔隙演化[J]. 吉林大学学报(地球科学版), 2016, 46(1): 23-35.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!