天然气地球科学

• 天然气地质学 • 上一篇    下一篇

东营凹陷北带沙四下亚段深层砂砾岩储层储集空间特征及成因机制

王淑萍,徐守余,董春梅,王丽萍     

  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.中国石化胜利油田东胜集团股份公司,山东 东营 257000
  • 收稿日期:2013-08-09 修回日期:2013-10-14 出版日期:2014-08-10 发布日期:2014-08-10
  • 作者简介:王淑萍(1978-),女,甘肃民勤人,博士研究生,主要从事油气储层评价研究. E-mail:wshpwyzh0619@163.com.
  • 基金资助:
    国家科技重大专项(编号:2011ZX05009-003);中央高校基本科研业务费专项资金项目(编号:12CX04001A;13CX02035A)联合资助.
     

Reservoir-space Characteristics and Genetic Mechanism of Deep Glutenite Reservoirof  Esx4  in the North Zone of the Dongying Depression

WANG Shu-ping,XU Shou-yu,DONG Chun-mei,WANG Li-ping   

  1. 1.School of Geosciences in China University of Petroleum,Qingdao 266580,China;
    2.Dongsheng Group Co.,Ltd.of Shengli Oil Field,SINOPEC,Dongying 257000,China
  • Received:2013-08-09 Revised:2013-10-14 Online:2014-08-10 Published:2014-08-10

摘要:

东营凹陷民丰洼陷北带沙四下亚段深层砂砾岩储层储集空间特征及成因机制认识不清的问题,给该地区油气勘探带来了极大的风险。综合运用薄片鉴定、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,结合压力演化史、油气成藏史、有机质热演化史等研究成果,对东营凹陷北带沙四下亚段砂砾岩储层储集空间特征及成因机制进行了系统研究。结果表明,东营凹陷北带沙四下亚段砂砾岩储层储集空间以残余原生孔隙为主,相对含量占60%以上,含有少量的次生溶蚀孔隙及微裂缝。在早期异常高压、早期油气充注以及膏岩层的发育等多种因素的综合作用下,东营凹陷北带沙四下亚段砂砾岩储层原生孔隙得以有效的保存至深层,从而为油气聚集提供了优质的储集空间;沙四下亚段深层砂砾岩储层经历了酸性→碱性→酸性的溶解过程,溶解作用相对较弱,次生孔隙含量低,对储层物性的贡献量小。
 

关键词: 储集空间, 成因机制, 沙四下亚段, 砂砾岩体, 东营凹陷北带

Abstract:

The reservoir-space characteristics and its genetic mechanism of deep glutenite reservoir in the lower part of the fourth member of the Shahejie Formation(Esx4 )in the north zone of the Minfeng Sag in the Dongying Depression haven′t been clearly understood,and it has brought out great risks to hydrocarbon exploration.Based on a combination of thin-section identification,scanning electron microscope(SEM)observation,fluid inclusion analysis and an analysis of core properties,in addition to knowledge on the pressure evolution history,the history of hydrocarbon accumulation and the thermal evolution of organic matters,systematic study has been carried out about the reservoir-space characteristics and its genetic mechanism of glutenite reservoir in Esx4 in the north zone of the Dongying Depression.The reservoir-space of glutenite reservoir is mainly residual primary pores in Esx4  in the north zone of the Dongying Depression whose relative content is more than 60%,with a small amount of secondary dissolution-pores and microcrack.As a result of the combination of early abnormal high pressure,early hydrocarbon-filling as well as the development of gypsum-salt bed,the primary pores of the glutenite reservoir in Esx4in the north zone of the Dongying Depression are effectively reserved to the deep,which has provided high-quality reservoir-space for hydrocarbon-accumulation.The glutenite reservoir has experienced the dissolution process of “acid-alkaline-acid”,and the dissolution is weaker with a small amount of secondary pores,which contributes little to its physical properties.

Key words: Reservoir space;Genetic mechanism, Esx4, Glutenite body, North zone of the Dongying Depression

中图分类号: 

  • TE122.2+3

[1]Zhu Xiaomin,WangYingguo,Zhong Dakang, et al. Pore types and secondary pore evolution of Paleogene Reservoir in the Jiyang Sag[J].Acta GeologicaSinica,2007,81(2):197-204.[朱筱敏,王英国,钟大康,等.济阳坳陷古近系储层孔隙类型与次生孔隙成因[J].地质学报,2007,81(2):197-204.]
 [2]Chen Yongqiao,Yu Xinghe,Zhou Xingui, et al. Research on diagenetic evolutive succession and occurrence of secondary porosity of Lower Tertiary in different structural belt of Dongying Depression[J].Natural Gas Geoscience,2004,15(1):68-74.[陈永峤,于兴河,周新桂,等.东营凹陷各构造区带下第三系成岩演化与次生孔隙发育规律研究[J].天然气地球科学,2004,15(1):68-74.]
 [3]Yuan Jing.Diagenesis and secondary pore development in Paleogene deep formation in Dongying Sag[J].Coal Geology & Exploration,2003,31(3):20-23.[袁静.东营凹陷下第三系深层成岩作用及次生孔隙发育特征[J].煤田地质与勘探,2003,31(3):20-23.]
 [4]Yuan Jing,Zhang Shanwen,Qiao Jun, et al. Cause of formation and dynamic mechanisms in multiply medium of dissolved pores in deep formation of Dongying Sag[J].Acta Sedimentologica Sinica,2007,25(6):840-846.[袁静,张善文,乔俊,等.东营凹陷深层溶蚀孔隙的多重介质成因机理和动力机制[J].沉积学报,2007,25(6):840-846.]
 [5]Li Guangyun,Lai Fuqiang,He Jiacheng, et al. Reservoir characteristic and controlling factors on physical properties of Lower Jurassic tight sandstone in the Qiudong Sag[J].Natural Gas Geoscience,2013,24(2):310-319.[李光云,赖富强,何加成,等.吐哈盆地丘东洼陷下侏罗统致密砂岩储层特征及物性主控因素[J].天然气地球科学,2013,24(2):310-319.]
 [6]Lian Chengbo,Zhong Jianhua,Yang Yufang, et al. Influence of Quan 4 Formation sandstone diagenesis on reservoir properties in Longxi region,Songliao Basin[J].Natural Gas Geoscience,2009,20(5):691-694.[连承波,钟建华,杨玉芳,等.松辽盆地龙西地区泉四段砂岩成岩作用对储层物性的影响[J].天然气地球科学,2009,20(5):691-694.]
 [7]Jin Zhenkui,Su Kui,Su Nina.Origin of Jurassic deep burial high-quality reservoirs in the central Junggar Basin[J].ActaPetrolei Sinica,2011,32(1):25-31.[金振奎,苏奎,苏妮娜.准噶尔盆地腹部侏罗系深部优质储层成因[J].石油学报,2011,32(1):25-31.]
 [8]Zhong Dakang,Zhu Xiaomin.Reservoirs characteristics and formation mechanism of high quality reservoirs in Kela-2 Gasfield[J].Natural Gas Industry,2007,27(1):8-11.[钟大康,朱筱敏.克拉2气田储层特征及优质储层形成机理[J].天然气工业,2007,27(1):8-11.]
 [9]Salman B,Robert H L,Linda B.Anomalously high porosity and permeability in deeply buried sandstone reservoirs:Origin and predictability[J].AAPG Bulletin,2002,86(2):301-328.[10]Wang Yanzhong.Genetic Mechanism and Evolution Model of Secondary Pore Development Zone of Paleogene in the North Zone in Dongying Depression[D].Qingdao :China University of Petroleum,2010.[王艳忠.东营凹陷北带古近系次生孔隙发育带成因机制及演化模式[D].青岛:中国石油大学(华东),2010.][11]Wang Yanzhong,Cao Yingchang,Li Yongxin, et al. Controlling factor on the paleogene deep effective reservoirs in the Bonan Sag[J],Natural Gas Geoscience,2012,23(6):996-1003.[王艳忠,操应长,李永新,等.渤南洼陷古近系深层有效储层控制因素研究[J].天然气地球科学,2012,23(6):996-1003.]
 [12]Zhong Jianhua,Wang Guozhuang,Gao Xiangcheng, et al. Sedimentary features,genesis and relation to hydrocarbon of fan-anticline in the north slope of the Dongying Sag[J].Chinese Journal ofGeology,2004,43(4):625-636.[钟建华,王国壮,高祥成,等.东营凹陷北部陡坡带丰1扇背斜的特征、成因及其与油气的关系[J].地质科学,2004,43(4):625-636.]
 [13]Zhang Yonggang,Xu Weiping,Wang Guoli, et al. Oil and Gas Accumulation Assembly of Continental fault Basin in East China[M].Beijing:Petroleum Industry Press,2006:127-131.[张永刚,许卫平,王国力,等.中国东部陆相断陷盆地油气成藏组合体[M].北京:石油工业出版社,2006:127-131.]
 [14]Wan Nianming,Wang Yanzhong,Cao Yingchang, et al. Overpressured fluid compartment and hydrocarbon accumulation of deep layer of Es4 in the north zone of Minfeng Sag,Dongying Depression[J].Acta Sedimentologica Sinica,2010,28(2):395-400.[万念明,王艳忠,操应长,等.东营凹陷民丰洼陷北带沙四段深层超压封存箱与油气成藏[J].沉积学报,2010,28(2):395-400.]
 [15]Sui Fenggui,Cao Yingchang,Liu Huimin, et al. Physical properties evolution and hydrocarbon accumulation of Paleogene nearshore subaqueous fan in the dastern north margin of the Dongying Depression[J].Acta Geologica Sinica,2010,84(2):246-256.[隋风贵,操应长,刘惠民,等.东营凹陷北带东部古近系近岸水下扇储集物性演化及其油气成藏模式[J].地质学报,2010,84(2):246-256.]
 [16]Pu Xiugang,Zhou Lihong,Wang Wenge, et al. Medium-deep clastic reservoirs in the slope area of Qikou Sag,Huanghua Depression,Bohai Bay Basin[J].Petroleum Exploration and Development,2013,40(1):36-48.[蒲秀刚,周立宏,王文革,等.黄骅坳陷歧口凹陷斜坡区中深层碎屑岩储集层特征[J].石油勘探与开发,2013,40(1):36-48.]
 [17]Sun Xiuli.Hydrocarbon Charging Mechanism and Reservoir Forming Models in the Deep Formations of North Belt,Dongying Depression[D].Beijing:China University of Geosciences,2010.[孙秀丽.东营凹陷北带深层油气充注机理及成藏模式研究[D].北京:中国地质大学,2010.]
 [18]Du Xiaodi,Yao Chao.The necesarry need of deep oil and gas exploration[J].Marine Oil and Gas Geology,2001,6(1):1-5.[杜小弟,姚超.深层油气勘探势在必行[J].海相油气地质,2001,6(1):1-5.]
 [19]Shou Jianfeng.Dynamic Mechanisms and Models of Sandstone Compaction in Oil and Gas Basin in Northern China[D].Beijing:China Petroleum Exploration and Development Research Institute,2004:42-47.[寿建峰.中国北方油气盆地砂岩成岩压实作用的动力成因机制与模式[D].北京:中国石油勘探开发研究院,2004:42-47.]
 [22]Wang Shuping.Diagenesis Researches of Natural Gas Reservoir with Gyprock And Salt Bed in Minfeng Area of the lower Part of Number 4 of Sha Hejie Formation in Dongying Depression[D].Dongying:China University of Petroleum,2007.[王淑萍.东营凹陷民丰地区沙四下亚段膏盐层系天然气储层成岩作用研究[D].东营:中国石油大学(华东),2007.]
 [21]Surdam R C,Boese S W,Crossey G J.The chemistry of secondary porosity[J].AAPG Memoir,1984,37:127-151.
 [22]Surdam R C,Crossey L J,Hagen E S.Organic-inorganic and sandstone diagenesis[J].AAPG Bulletin,1989,73:1-23.

[1] 张云钊,曾联波,罗群,张晨,吴浩,吕文雅,代全齐,朱德宇. 准噶尔盆地吉木萨尔凹陷芦草沟组致密储层裂缝特征和成因机制[J]. 天然气地球科学, 2018, 29(2): 211-225.
[2] 杨志冬. 准噶尔盆地红山嘴油田红153井区二叠系夏子街组砂砾岩储层特征及影响因素[J]. 天然气地球科学, 2017, 28(12): 1829-1838.
[3] 王淑芳,张子亚,董大忠,王玉满,李新景,胡俊文,黄金亮,管全中. 四川盆地下寒武统筇竹寺组页岩孔隙特征及物性变差机制探讨[J]. 天然气地球科学, 2016, 27(9): 1619-1628.
[4] 梅庆华,何登发,桂宝玲,李英强,李皎,李传新. 川中地区新元古代—古生代初多幕裂陷过程及其演化[J]. 天然气地球科学, 2016, 27(8): 1427-1438.
[5] 刘一锋,邱楠生,谢增业,姚倩颖,刘雯. 川中古隆起寒武系超压形成与保存[J]. 天然气地球科学, 2016, 27(8): 1439-1446.
[6] 刘金库,孙永亮,焦旭,张泽. 碎屑岩储层低渗成因及优质储层发育机理——以歧口凹陷歧北斜坡沙二段储层为例[J]. 天然气地球科学, 2016, 27(5): 799-808.
[7] 郑剑锋,陈永权,倪新锋,严威,黄理力,张艳秋. 基于CT成像技术的塔里木盆地寒武系白云岩储层微观表征[J]. 天然气地球科学, 2016, 27(5): 780-789.
[8] 李恒超,刘大永,彭平安,王庆涛. 构造作用对重庆及邻区龙马溪组页岩储集空间特征的影响[J]. 天然气地球科学, 2015, 26(9): 1705-1711.
[9] 郑剑锋,沈安江,陈永权,倪新锋,张先龙. 塔里木盆地下古生界白云岩储集空间特征及储层分类探讨[J]. 天然气地球科学, 2015, 26(7): 1256-1267.
[10] 王香增,刘国恒,黄志龙,孙兵华,史鹏,杨潇. 鄂尔多斯盆地东南部延长组长7段泥页岩储层特征[J]. 天然气地球科学, 2015, 26(7): 1385-1394.
[11] 吴斌,何登发,孙方源. 塔里木盆地古城低凸起下古生界的断裂特征及成因机制[J]. 天然气地球科学, 2015, 26(5): 871-879.
[12] 王圣柱,林会喜,张奎华,吴倩倩. 准北缘哈山斜坡带侏罗系原油稠化机理及充注特征[J]. 天然气地球科学, 2015, 26(3): 477-485.
[13] 张顺,陈世悦,鄢继华,谭明友,张云银,龚文磊,王光增. 东营凹陷西部沙三下亚段—沙四上亚段泥页岩岩相及储层特征[J]. 天然气地球科学, 2015, 26(2): 320-332.
[14] 远光辉,操应长,贾珍臻,王艳忠,杨田. 含油气盆地中深层碎屑岩储层异常高孔带研究进展[J]. 天然气地球科学, 2015, 26(1): 28-42.
[15] 葸克来,操应长,赵贤正,周磊,金凤鸣,金杰华,董雄英. 霸县凹陷古近系中深层有效储层成因机制[J]. 天然气地球科学, 2014, 25(8): 1144-1155.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!