天然气地球科学 ›› 2010, Vol. 21 ›› Issue (6): 1057–1060.doi: 10.11764/j.issn.1672-1926.2010.06.1057

• 煤层气 • 上一篇    

煤层气与页岩气聚集主控因素对比

姜文利, 赵素平, 张金川, 叶欣   

  1. 1.中国地质大学(北京)能源学院海相储层演化与油气富集机理教育部重点实验室,北京 100083;
    2.国土资源部油气资源战略研究中心,北京 100034;3.中国石油勘探开发研究院廊坊分院,
    河北 廊坊 065007;4.中国石油化工股份有限公司石油勘探开发研究院,北京 100083
  • 收稿日期:2010-01-15 修回日期:2010-05-06 出版日期:2010-12-10 发布日期:2010-12-10
  • 通讯作者: 姜文利jwl1980@126.com E-mail:jwl1980@126.com
  • 作者简介:姜文利(1980-),男,黑龙江绥化人,助理研究员,在读博士,主要从事石油地质、煤层气、页岩气、油气资源基础科研及战略研究.
  • 基金资助:

    国家自然科学基金(编号:40672087;40472073)联合资助.

Comparison of Controlled Factors for Coalbed Methane and Shale Gas Accumulation

JIANG Wen-Li, ZHAO Su-Ping, ZHANG Jin-Chuan, YE Xin   

  1. 1.School of Energy Resources,Key Laboratory of Marine Reservoir Evolution and Hydrocarbon
    AccumulationMechanism,Ministry of Education,China University of Geosciences (Beijing),Beijing 100034,China;
    2.Strategic Research Center of Oil and Gas Resources,Ministry of Land and Resources,Beijing 100083,China;
    3.Langfang Branch,Research Institute of Petroleum Exploration and Development,PetroChina,Langfang  065007,China;
    4.Exploration and Production Research Institute,SINOPEC,Beijing100083,China
  • Received:2010-01-15 Revised:2010-05-06 Online:2010-12-10 Published:2010-12-10

摘要:

我国已进入煤层气产业快速发展,页岩气开发迅速起步阶段。国内外一些典型盆地均出现煤层气与页岩气混合共生的现象,研究两者共性及差异性对指导勘探开发具有重要意义。煤层气与页岩气在形成背景、气源、储集等诸多方面存在共性(两者富集成藏均受厚度、热成熟度、有机质含量和储层孔隙、微裂隙发育等因素控制)和差异性(煤层气还受构造和水文地质等条件影响明显)。在沉积环境方面,煤层主要形成于滨海或滨湖平原、三角洲平原、冲积平原及冲积扇前缘等沉积环境,而页岩则形成于快速沉积且封闭性较好的还原环境。

关键词: 煤层气, 页岩气, 聚集主控因素, 混合沉积

Abstract:

It is rapid development of CBM in China,in contrast shale gas is starting.It is important to elucidate the common and difference between CBM and shale gas,because of similar aspects of gas sources,migration,preservation and accumulation between them.There is mixing of CBM and shale gas in some basins.The accumulation of both gases is constrained by reservoir thickness,thermal maturity,organic matter content,and reservoir pore and microfracture.The CBM is also affected by structure and hydrogeology.By contrast of depositional conditions,the coal was mainly formed in the seashore,delta plain,alluvial plain and front of alluvial fan,while the shale was quickly deposited in the reductive environment.

Key words: Coalbed methane, Shale gas, Hydrocarbon accumulation, Mixed sedimentation

中图分类号: 

  •  

[1]Zhang Jinchuan,Jin Zhijun,Yuan Mingsheng,et al.Reservoiring mechanism of shale gas and its distribution[J].Natural Gas Industry,2004,24(7):51-58.[张金川,金之钧,袁明生,等.页岩气成藏机理和分布[J].天然气工业,2004,24(7):51-58.]
[2]Zhang Jinchuan,Xue Hui,Zhang Deming,et al.Reservoiring mechanism of shale gas[J].Geoscience,2003,17(4):466.[张金川,薛会,张德明,等.页岩气及其成藏机理[J].现代地质,2003,17(4):466.] 
[3]Li Denghua,Li Jianzhong,Wang Shejiao,et al.Analysis of controls on gas shale reservoirs[J].Natural Gas Industry,2009,29(5):22-26.[李登华,李建忠,王社教,等.页岩气藏形成条件分析[J].天然气工业,2009,29(5):22-26.] 
[4]Zhao Qun,Wang Hongyan,Li Jingming,et al.Forming differences between high and low coal rank coalbed methane reservoirs[J].Natural Gas Geoscience,2007,18(1):129-133.[ 赵群,王红岩,李景明,等.我国高低煤阶煤层气成藏的差异性[J].天然气地球科学,2007,18(1):129-133.]
[5]Li Xinjing,Lü Zonggang,Dong Dazhong,et al.Geologic controls on accumulation of shale gas in north America[J].Natural Gas Industry,2009,29(5):27-39.[李新景,吕宗刚,董大忠,等.北美页岩气资源形成的地质条件[J].天然气工业,2009,29(5):27-39.]
[6]Li Guizhong,Wang Hongyan,Wu Lixin,et al.Theory of syncline-controlled coalbed methane[J].Natural Gas Industry,2005,25(1):26-28.[李贵中,王红岩,吴立新,等.煤层气向斜控气论[J].天然气工业,2005,25(1):26-28.] 
[7]Liu Honglin,Li Jingming,Wang Hongyan,et al.Different effects of hydrodynamic conditions on coalbed gas accumulation.[J].天然气工业,2006,26(3):35-37.[刘洪林,李景明,王红岩,等.水动力对煤层气成藏的差异性研究[J].天然气工业,2006,26(3):35-37.]
[8]Chen Gengsheng,Dong Dazhong,Wang Shiqian,et al.A preliminary study on accumulation mechanism and enrichment pattern of shale gas[J].Natural Gas Industry,2009,29(5):17-21.[陈更生,董大忠,王世谦,等.页岩气藏形成机理与富集规律初探[J].天然气工业,2009,29(5):17-21.]
[9]Wang Hongyan,Liu Honglin,Liu Huaiqing,et al.The technique and application of coalbed methane reservoir physical simulation[J].Natural Gas Geoscience,2004,15(4):349-351.[王红岩,刘洪林,刘怀庆,等.煤层气成藏模拟技术及应用[J].天然气地球科学,2004,15(4):349-351.]
[10]Qin Yong,Song Quanyou,Fu Xuehai.Discussion on reliability for co-mining the coalbed gas and normal petroleum and natural gas:Absorptive effect of deep coal reservoir under condition of balanced water[J].Natural Gas Geoscience,2005,16(4):492-498.[秦勇,宋全友,傅雪海.煤层气与常规油气共采可行性探讨——深部煤储层平衡水条件下的吸附效应[J].天然气地球科学,2005,16(4):492-498.]

 

[1] 赵文韬,荆铁亚,吴斌,周游,熊鑫. 断裂对页岩气保存条件的影响机制——以渝东南地区五峰组—龙马溪组为例[J]. 天然气地球科学, 2018, 29(9): 1333-1344.
[2] 夏鹏,王甘露,曾凡桂,牟雨亮,张昊天,刘杰刚. 黔北地区牛蹄塘组高—过成熟页岩气富氮特征及机理探讨[J]. 天然气地球科学, 2018, 29(9): 1345-1355.
[3] 吴丛丛,杨兆彪,孙晗森,张争光,李庚,彭辉. 云南恩洪向斜西南区垂向流体能量特征及有序开发建议[J]. 天然气地球科学, 2018, 29(8): 1205-1214.
[4] 康毅力,豆联栋,游利军,陈强,程秋洋. 富有机质页岩增产改造氧化液浸泡离子溶出行为[J]. 天然气地球科学, 2018, 29(7): 990-996.
[5] 曾凡辉,王小魏,郭建春,郑继刚,李亚州,向建华. 基于连续拟稳定法的页岩气体积压裂水平井产量计算[J]. 天然气地球科学, 2018, 29(7): 1051-1059.
[6] 朱维耀,马东旭. 页岩储层有效应力特征及其对产能的影响[J]. 天然气地球科学, 2018, 29(6): 845-852.
[7] 余川,曾春林,周洵,聂海宽,余忠樯. 大巴山冲断带下寒武统页岩气构造保存单元划分及分区评价[J]. 天然气地球科学, 2018, 29(6): 853-865.
[8] 邱 振,邹才能,李熙喆,王红岩,董大忠,卢斌,周尚文,施振生,冯子齐,张梦琪. 论笔石对页岩气源储的贡献——以华南地区五峰组—龙马溪组笔石页岩为例[J]. 天然气地球科学, 2018, 29(5): 606-615.
[9] 汪道兵,葛洪魁,宇波,文东升,周珺,韩东旭,刘露. 页岩弹性模量非均质性对地应力及其损伤的影响[J]. 天然气地球科学, 2018, 29(5): 632-643.
[10] 龙胜祥,冯动军,李凤霞,杜伟. 四川盆地南部深层海相页岩气勘探开发前景[J]. 天然气地球科学, 2018, 29(4): 443-451.
[11] 贺领兄,宋维刚,安生婷,徐永锋,沈娟,路超,王军. 青海东昆仑地区八宝山盆地烃源岩有机地球化学特征与页岩气勘探前景[J]. 天然气地球科学, 2018, 29(4): 538-549.
[12] 邢 舟,曹高社,毕景豪,周新桂,张交东. 南华北盆地禹州地区ZK0606钻孔上古生界煤系烃源岩评价[J]. 天然气地球科学, 2018, 29(4): 518-528.
[13] 卢文涛,李继庆,郑爱维,梁榜,张谦,杨文新. 涪陵页岩气田定产生产分段压裂水平井井底流压预测方法[J]. 天然气地球科学, 2018, 29(3): 437-442.
[14] 鲍祥生,谈迎,吴小奇,郑红军. 利用纵横波速度法预测泥页岩脆性矿物指数[J]. 天然气地球科学, 2018, 29(2): 245-250.
[15] 梁榜,李继庆,郑爱维,卢文涛,张谦. 涪陵页岩气田水平井开发效果评价[J]. 天然气地球科学, 2018, 29(2): 289-295.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!