天然气地球科学

• 天然气地质学 • 上一篇    下一篇

松辽盆地英台断陷天然气资源潜力探讨

郑曼1,李建忠1,王颖2,陈晓明1,范晶2,郑民1,吴晓智1,王文广3   

  1. 1.中国石油勘探开发研究院,北京100083;
    2.中国石油吉林油田公司勘探开发研究院,吉林 松原 138000;
    3.中国石油大学(华东)非常规油气与新能源研究院,山东 青岛 266580
  • 收稿日期:2016-06-10 修回日期:2016-07-22 出版日期:2016-09-10 发布日期:2016-09-10
  • 作者简介:郑曼(1981-),女,湖北黄冈人,高级工程师,主要从事石油地质研究. E-mail:zhm2007@petrochina.com.cn.
  • 基金资助:
    中国石油重大科技专项“中国石油第四次油气资源评价”(编号:2013E-050201)资助.

Gas resource potential in Yingtai fault depression of southern Songliao Basin

Zheng Man1,Li Jian-zhong1,Wang Ying2,Chen Xiao-ming1,Fan Jing2,Zheng Min1,Wu Xiao-zhi1,Wang Wen-guang3   

  1. 1.Research Institute of Petroleum Exploration & Development,CNPC,Beijing 100083,China;
    2.Exploration and Development Research Institute of Jilin Oilfield Company,PetroChina, Songyuan 138000,China;
    3.Institute of Unconventional Hydrocarbon and New Energy,China University of Petroleum,Qingdao 266580,China
  • Received:2016-06-10 Revised:2016-07-22 Online:2016-09-10 Published:2016-09-10

摘要: 英台断陷发育营城组一段火山岩岩性—构造气藏,营城组二段致密沉火山碎屑岩岩性气藏及登娄库组—泉头组砂岩气藏3种类型气藏。在分析气藏特征与成藏主控因素的基础上,指出了每种类型气藏的分布规律,并针对不同类型气藏分别采用特尔非法、容积法及地质分析类比法计算了天然气资源量。评价结果表明,英台断陷天然气总资源量为2 848×108m3,剩余资源量为2 228×108m3,占总资源量的78%,其中营城组二段的致密沉火山碎屑岩气藏资源探明率仅为18%,剩余资源潜力大,为下一步勘探的重要接替领域。

关键词: 构造—岩性气藏, 沉火山碎屑岩, 成藏主控因素, 天然气资源量, 英台断陷

Abstract: There are three kinds of gas reservoirs in the Yingtai fault depression,southern Songliao Basin:Structure-lithology reservoir in the volcanic rock of the Yingcheng-1 Formation,lithology reservoir in the sedimentary pryoclastics rock of the Yingcheng-2 Formation and sand stone reservoir in the Denglouku-Quantou Formations.Based on analysis of the gas pool features and controlling factors,distribution of each kind has been studied.The resources of these gas reservoirs have been estimated by Delphi method,volumetric method and geological analytical analogy method,respectively.The results of the resources assessment show the total gas resources of the Yingtai fault depression is 284.8bcm,while the remaining is 222.8bcm,accounting for 78%.Especially,the exploration proven rate is only 18% for the lithology gas pool in the sedimentary pryoclastics rock of the Yingcheng-2 member,thus there will be great exploration potential in the future.

Key words: Structure-lithology gas pool, Sedimentary pryoclastics rock, Gas pool-formation controlling factors, Gas resources, Yingtai fault depression

中图分类号: 

  • TE122.2

[1]Du Jinhu.Gas Exploration in Mesozoic Volcanic Reservoirs of Songliao Basin[M].Beijing:Petroleum Industry Press,2010:1-187.[杜金虎.松辽盆地中生界火山岩天然气勘探[M].北京:石油工业出版社,2010:1-187.]
[2][KG*6/7]Lin Shiguo,Zhao Zehui,Xu Shujuan,et al.Enrichment and exploration prospects in deep volcanic gas reservoirs in Songliao Basin[J].Xinjiang Petroleum Geology,2013,34(2):174-178.[林世国,赵泽辉,徐淑娟,等.松辽盆地深层火山岩气藏富集规律与勘探前景[J].新疆石油地质,2013,34(2):174-178.][JP]
[3]Wu Guoqing.The Research of Natural Gas Accumulation in Yingcheng Formation of Yingtai Fault Depression[D].Daqing:Northeast Petroleum University,2013:4-19.[吴国庆.英台断陷营城组天然气成藏条件研究[D].大庆:东北石油大学,2013:4-19.]
[4]Wang Pujun,Feng Zhiqiang.Volcanic Rocks in Basin:Lithology,Llithofacies,Reservoirs,Gas Accumulation,Exploration[M].Beijing:Science Press,2007:1-169.[王璞珺,冯志强.盆地火山岩:岩性·岩相·储层·气藏·勘探[M].北京:科学出版社,2007:1-169.]
[5]Xie Zhou.Analysising the Gas Reservoir Forming Conditions and Forecasting for Favorable Areas Yingcheng Formation in Yingtai Fault Depression[D].Daqing:Northeast Petroleum University,2014:25-42.[谢舟.英台断陷营城组天然气成藏条件分析及有利区预测[D].大庆:东北石油大学,2014:25-42.][JP]
[6]Huang Wenbiao,Lu Shuangfang,Xue Haitao,et al.Causes analysis of deep natural gas and correlation of gas source in Yingtai fault depression[J].Science Technology and Engineering,2011,11(9):1944-1950.[黄文彪,卢双舫,薛海涛,等.英台断陷深层天然气成因分析及气源对比[J].科学技术与工程,2011,11(9):1944-1950.]
[7]Lu Shuangfang,Hu Huiting,Liu Haiying,et al.Gas source conditions and exploration potential of deep layer in Yingtai fault depression[J].Journal of Jilin University:Earth Science Edition,2010,40(4):912-919.[卢双舫,胡慧停,刘海英,等.英台断陷深层的气源条件及勘探潜力[J].吉林大学学报:地球科学版,2010,40(4):912-919.]
[8]Dobson P F,Kneafsey T J,Hulen J,et al.Porosity,permeability,and fluid flow in the Yellowstone geothermal system,Wyoming[J].Journal of volcanology and Geothermal Research,2003,123:313-324.
[9]Batchor A S.Hydrocarbon Production from Fractured Basement Formation [R].Geoscience Ltd.Fahnouth,Cornwall.Online publication.Version 6.2000.
[10]Hart A.New Zealand potential[J].Oil & Gas Journal,2001,99(29):38-44.
[11]Zheng Man,Li Jianzhong,Wang Liwu,et al.Reservoir space characteristics and evolution of the volcanic rocks in Yingcheng Formation of Changling fault depression,Songliao Basin[J].Acta Petrologica Sinica,2010,26(1):135-141.[郑曼,李建忠,王立武,等.松辽盆地长岭断陷营城组火山岩储集空间特征及演化[J].岩石学报,2010,26(1):135-141.]
 [12]Zhao Wenzhi,Zou Caineng,Li Jianzhong,et al.Comparative study on volcanic hydrocarbon accumulations in western and eastern China and its significance[J].Petroleum Exploration & Development,2009,36(1):1-10.[赵文智,邹才能,李建忠,等.中国陆上东、西部地区火山岩成藏比较研究与意义[J].石油勘探与开发,2009,36(1):1-10.]
[13]Zhang Li’na,Zhang Mingfeng,Wu Chenjun,et al.A review of the accumulation process and formation mechanism about different genetic types of tight-gas sandstone reservoir[J].Acta Sedimentologica Sinica,2015,33(5):1013-1022.[张丽娜,张明峰,吴陈君,等.不同成因类型致密砂岩气成藏过程及机理研究进展[J].沉积学报,2015,33(5):1013-1022.]
[14]Wei Guoqi,Zhang Fudong,Li Jun,et al.New progress of tight sand gas accumulation theory and favorable exploration zones in China[J].Natural Gas Geoscience,2016,27(2):199-210.[魏国齐,张福东,李君,等.中国致密砂岩气成藏理论进展[J].天然气地球科学,2016,27(2):199-210.]
[15]Dong Yuexia,Pang Xiongqi,Guo Jigang,et al.Accumulation conditions of tight sand gas in the 3rd member of the Shahejie Formation in Nanpu Sag,Bohai Bay Basin[J].Oil & Gas Geology,2015,36(1):23-34.[董月霞,庞雄奇,郭继刚,等.南堡凹陷沙三段致密砂岩气成藏条件[J].石油与天然气地质,2015,36(1):23-34.]
 [16]Zou Caineng,Tao Shizhen,Yuan Xuanjun,et al.Global importance of “continuous” petroleum reservoirs:Accumulation,distribution and evaluation[J].Petroleum Exploration and Development,2009,36(6):669-682.[邹才能,陶士振,袁选俊,等.连续型油气藏及其在全球的重要性:成藏、分布与评价[J].石油勘探与开发,2009,36(6):669-682.]
[17]Li Jianzhong,Guo Bincheng,Zheng Min,et al.Main types,geological features and resource potential of tight sandstone gas in China[J].Natural Gas Geoscience,2012,23(4):607-615.[李建忠,郭彬程,郑民,等.中国致密砂岩气主要类型、地质特征与资源潜力[J].天然气地球科学,2012,23(4):607-615.]

[1] 屈红军,张功成. 全球深水富油气盆地分布格局及成藏主控因素[J]. 天然气地球科学, 2017, 28(10): 1478-1487.
[2] 何家雄,张伟,卢振权,李晓唐. 南海北部大陆边缘主要盆地含油气系统及油气有利勘探方向[J]. 天然气地球科学, 2016, 27(6): 943-959.
[3] 吴亚东, 孙春岩, 王东旭, 蒋涛, 黄英, 龚建华. 哈萨克斯坦南图尔盖盆地南肯尼斯油田油气分布特征及成藏主控因素[J]. 天然气地球科学, 2016, 27(11): 2013-2022.
[4] 龚晓峰,何家雄,莫涛,陈胜红,张景茹,张伟,李晓唐. 珠江口盆地珠一坳陷惠陆油区含油气系统与油气运聚成藏模式[J]. 天然气地球科学, 2015, 26(12): 2292-2303.
[5] 李浩武,童晓光. 波斯湾盆地Khuff组成藏组合地质特征[J]. 天然气地球科学, 2012, 23(4): 727-735.
[6] 王拥军,张宝民,王政军,王旭东. 渤海湾盆地南堡凹陷奥陶系潜山油气地质特征与成藏主控因素[J]. 天然气地球科学, 2012, 23(1): 51-59.
[7] 李军, 陶士振, 汪泽成, 邹才能, 高晓辉, 王世谦. 川东北地区侏罗系油气地质特征与成藏主控因素[J]. 天然气地球科学, 2010, 21(5): 732-741.
[8] 张凤敏;魏国齐;李剑;郭晋华;胡国艺;石强 . 柴达木盆地东部水溶性天然气层分类及成藏主控因素研究[J]. 天然气地球科学, 2008, 19(06): 882-887.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 朱俊章;施和生;舒誉;杜家元;罗俊莲;. 珠江口盆地珠-坳陷典型烃源岩热压模拟实验――生排烃模式及TOC恢复系数探讨[J]. 天然气地球科学, 2006, 17(4): 573 -578 .
[2] 王晓锋;刘文汇;刘全有;张殿伟;南青云;. 有机体及其沉积演化产物的氢同位素地球化学研究进展[J]. 天然气地球科学, 2004, 15(3): 311 -316 .
[3] 郑军卫. 1991~2000年世界天然气生产一览表(108m3)[J]. 天然气地球科学, 2002, 13(3-4): 73 -81 .
[4] 王宏波, 郑希民,冯 明. 鄂尔多斯盆地三叠系延长组层序地层与生储盖组合特征[J]. 天然气地球科学, 2006, 17(5): 677 -681 .
[5] 胡 斌,李广之,吴向华,邓天龙 . 岩屑荧光录井技术及荧光指标量化方法[J]. 天然气地球科学, 2007, 18(1): 121 -124 .
[6] S.R.Dallimore;T.S.Collett;王万春;. 加拿大马更些三角洲西北部永冻层的气水合物[J]. 天然气地球科学, 1998, 9(3-4): 32 -36 .
[7] Г.Д.Гинсбург;И.С.Грамберг;В.А.Соловьев;史斗;. 陆坡气水合物[J]. 天然气地球科学, 1998, 9(3-4): 54 -56 .
[8] 任以发;. 黄桥二氧化碳气田成藏特征与进一步勘探方向[J]. 天然气地球科学, 2005, 16(5): 632 -636 .
[9] 陈启林;杨占龙;关银录;卫平生;. 银根-额济纳裂谷盆地群凹陷结构样式及对成藏的控制[J]. 天然气地球科学, 2005, 16(5): 559 -563 .
[10] 孙德强;张涛;梁彬;祁文珍;刘健;翟志锋;杨联系;刘志舟;赵凡 . 柴达木盆地北缘油气成藏特征[J]. 天然气地球科学, 2008, 19(05): 652 -656 .