松辽盆地南部英台断陷营城组火山岩晶间微孔特征及储层效应

doi:10.7623/syxb201304006

石油学报 ›› 2013, Vol. 34 ›› Issue (4): 667-674.DOI: 10.7623/syxb201304006

松辽盆地南部英台断陷营城组火山岩晶间微孔特征及储层效应

高有峰¹, 吴艳辉^2,3, 刘万洙², 瞿雪姣², 唐华风²

1. 吉林大学古生物学与地层学研究中心吉林长春 130026;
2. 吉林大学地球科学学院吉林长春 130061;
3. 吉林省安全科学技术研究院吉林长春 130051

收稿日期:2013-02-12 修回日期:2013-05-07 出版日期:2013-07-25 发布日期:2013-07-04
通讯作者: 唐华风,男,1979年6月生,2001年获吉林大学学士学位,2007年获吉林大学博士学位,现为吉林大学副教授,主要从事火山岩储层地质、地球物理研究。Email:tanghfhc@jlu.edu.cn
作者简介:高有峰,男,1982年6月生,2004年获吉林大学学士学位,2010年获吉林大学博士学位,现为吉林大学讲师,主要从事火山岩储层成岩作用和地层对比研究。Email:gaoyoufeng@jlu.edu.cn
基金资助:
国家重点基础研究发展计划(973)项目(2012CB822002和2009CB219305)和国家自然科学基金项目(No.41002038)资助。

Intercrystalline micropore characteristics and reservoir effect of Yingcheng Formation volcanic rock in Yingtai fault depression, southern Songliao Basin

GAO Youfeng¹, WU Yanhui^2,3, LIU Wanzhu², QU Xuejiao², TANG Huafeng²

1. Research Center of Palaeontology & Stratigraphy, Jilin University, Changchun 130026, China;
2. College of Earth Sciences, Jilin University, Changchun 130061, China;
3. Jilin Academy of Safety Science & Technology, Changchun 130051, China

Received:2013-02-12 Revised:2013-05-07 Online:2013-07-25 Published:2013-07-04

摘要/Abstract

摘要：

松辽盆地南部英台断陷营城组火山岩中普遍发育晶间微孔隙,主要由重结晶作用和溶蚀作用形成。按成因和骨架颗粒的种类可将晶间微孔分为放射状碱性长石晶间微孔、黏土矿物晶间微孔和混合矿物晶间微孔3种类型。基质发生脱玻化重结晶作用,形成球粒状钾长石的区域晶间微孔面孔率为5.2%,形成黏土矿物和石英长石雏晶的区域面孔率增加9.5% ~13.6%;长石发生局部溶蚀形成伊利石的区域,面孔率可增加6.5% ~10.1%;而伊利石充填火山碎屑岩的粒间孔隙,仍可保留22.3% 的晶间微孔型储集空间。结合英台断陷勘探实例,认为晶间微孔发育的火山岩可作为天然气的有利储层。

关键词: 松辽盆地, 营城组, 火山岩, 晶间微孔, 成岩作用

Abstract:

Volcanic intercrystalline micropores mainly formed by recrystallization and dissolution develop widely in the Yingtai fault depression, southern Songliao Basin. According to the genesis and types of skeleton grains, volcanic intercrystalline micropores can be divided into three types, i.e. intercrystalline micropores of radial alkali feldspar, clay minerals and mixed minerals. Surface porosity analyses showed that due to the devitrification of matrix, the porosity of intercrystalline micropores in the spherulitic K-feldspar region amounts to 5.2%, the porosity of intercrystalline micropores in the region of clay minerals and quartz-feldspar crystallites increases from 9.5% to 13.5%, the porosity of intercrystalline micropores in the region where partial feldspar alters to illite may increase to 6.5% ~10.1%, while intergranular pores of pyroclastic rocks filled with illite can still retain a porosity of 22.3% for intercrystalline micropores. Combined with the exploration practice in the Yingtai fault depression, we suggested that volcanic rocks with rich intercrystalline micropores can serve as a favorable reservoir of natural gas.

Key words: Songliao Basin, Yingcheng Formation, volcanic rock, intercrystalline micropore, diagenesis

中图分类号:

TE112.222

高有峰, 吴艳辉, 刘万洙, 瞿雪姣, 唐华风. 松辽盆地南部英台断陷营城组火山岩晶间微孔特征及储层效应[J]. 石油学报, 2013, 34(4): 667-674.

GAO Youfeng, WU Yanhui, LIU Wanzhu, QU Xuejiao, TANG Huafeng. Intercrystalline micropore characteristics and reservoir effect of Yingcheng Formation volcanic rock in Yingtai fault depression, southern Songliao Basin[J]. Editorial office of ACTA PETROLEI SINICA, 2013, 34(4): 667-674.

参考文献

[1] 王璞珺,迟元林,刘万洙,等.松辽盆地火山岩相:类型、特征和储层意义[J].吉林大学学报:地球科学版,2003,33(4):449-456.

Wang Pujun,Chi Yuanlin,Liu Wanzhu,et al.Volcanic facies of the Songliao Basin:classification,characteristics and reservoir significance[J].Journal of Jilin University :Earth Science Edition,2003,33(4):449-456.

[2] 王璞珺,陈树民,刘万洙,等.松辽盆地火山岩岩相与火山岩储层的关系[J].石油与天然气地质,2003,24(1):18-23.

Wang Pujun,Chen Shumin,Liu Wanzhu,et al.Relationship between volcanic facies and volcanic reservoirs in SongLiao basin[J].Oil&Gas Geology,2003,24(1):18-23.

[3] 刘万洙,王璞珺,门广田,等.松辽盆地北部深层火山岩储层特征[J].石油与天然气地质,2003,24(1):28-31.

Liu Wanzhu,Wang Pujun,Men Guangtian,et al.Characteristics of deep volcanic reservoirs in northern Songliao Basin[J].Oil&Gas Geology,2003,24(1):28-31.

[4] 蒙启安,门广田,赵洪文,等.松辽盆地中生界火山岩储层特征及对气藏的控制作用[J].石油与天然气地质,2002,23(3):285-288.

Meng Qi'an,Men Guangtian,Zhao Hongwen,et al.Characteristics of Mesozoic volcanic rocks and its controlling effect on gas reservoir in Songliao Basin[J].Oil&Gas Geology,2002,23(3):285-288.

[5] 张方礼,尹万泉,郭建华,等.辽河大洼油田火山岩储层研究[M].武汉:中国地质大学出版社,2000:37-43.

Zhang Fangli,Yin Wanquan,Guo Jianhua,et al.Study on volcanic reservoirs of Dawa oilfield,Liaohe[M].Wuhan:China University of Geosciences Press,2000:37-43.

[6] 唐华风,白冰,边伟华,等.松辽盆地营城组火山机构地层结构定量模型[J].石油学报,2012,33(4):541-550.

Tang Huafeng,Bai Bing,Bian Weihua,et al.Quantitative models of strata texture within volcanic edifices of Yingcheng Formation in Songliao Basin,NE China[J].Acta Petrolei Sinica,2012,33(4):541-550.

[7] 唐华风,庞彦明,边伟华,等.松辽盆地白垩系营城组火山机构储层定量分析[J].石油学报,2008,29(6):841-845.

Tang Huafeng,Pang Yanming,Bian Weihua,et al.Reservoirs quantitative analysis of volcanic edifice of Yingcheng Formation in Songliao Basin,Early Cretaceous,NE China[J].Acta Petrolei Sinica,2008,29(6):841-845.

[8] 刘嘉麒,孟凡超,崔岩,等.试论火山岩油气藏成藏机理[J].岩石学报,2010,26(1):1-13.

Liu Jiaqi,Meng Fanchao,Cui Yan,et al.Discuss ion on the formation mechanism of volcanic oil and gas reservoirs[J].Acta Petrologica Sinica,2010,26(1):1-13.

[9] 侯启军.松辽盆地南部火山岩储层主控因素[J].石油学报,2011,32(5):749-756.

Hou Qijun.Main controlling factors of volcanic reservoirs in the southern Songliao Basin[J].Acta Petrolei Sinica,2011,32(5):749-756.

[10] 王璞珺,冯志强,刘万洙,等.盆地火山岩:岩性·岩相·储层·气藏·勘探[M].北京:科学出版社,2008:75-77.

Wang Pujun,Feng Zhiqiang,Liu Wanzhu,et al.Volcanic rocks in petroliferous basins:petrography·facie·reservoir·pool·exploration[M].Beijing:Science Press,2008:75-77.

[11] 王璞珺,吴河勇,庞彦明,等.松辽盆地火山岩相:相序、相模式与储层物性的定量关系[J].吉林大学学报:地球科学版,2006,36(5):805-812.

Wang Pujun,Wu Heyong,Pang Yanming,et al.Volcanic facies of the Songliao Basin:sequence,modeland the quantitative relationship with porosity & permeability of the volcanic reservoir[J].Journal of Jilin University :Earth Science Edition,2006,36(5):805-812.

[12] 罗静兰,侯连华,蒋宜勤,等.陆东地区火成岩形成时代与构造背景及火山岩储层成因[J].石油学报,2012,33(3):351-360.

Luo Jinglan,Hou Lianhua,Jiang Yiqin,et al.Chronology and tectonic settings of igneous rocks and origin of volcanic reservoirs in Ludong area,eastern Junggar Basin[J].Acta Petrolei Sinica,2012,33(3):351-360.

[13] 蔡东梅,孙立东,齐景顺,等.徐家围子断陷火山岩储层特征及演化规律[J].石油学报,2010,31(3):400-407.

Cai Dongmei,Sun Lidong,Qi Jingshun,et al.Reservoir characteristics and evolution of volcanic rocks in Xujiaweizi fault depression[J].Acta Petrolei Sinica,2010,31(3):400-407.

[14] 高有峰,刘万洙,纪学雁,等.松辽盆地营城组火山岩成岩作用类型、特征及其对储层物性的影响[J].吉林大学学报:地球科学版,2007,37(6):1251-1258.

Gao Youfeng,Liu Wanzhu,Ji Xueyan,et al.Diagenesis types and features of volcanic rocks and its impact on porosity and permeability in Yingcheng Formation,Songliao Basin[J].Journal of Jilin University:Earth Science Edition,2007,37(6):1251-1258.

[15] 杨双玲,刘万洙,于世泉,等.松辽盆地火山岩储层储集空间特征及其成因[J].吉林大学学报:地球科学版,2007,37(3):506-512.

Yang Shuangling,Liu Wanzhu,Yu Shiquan,et al.Pore textures and its causes of volcanic reservoir in Songliao Basin[J].Journal of Jilin University:Earth Science Edition,2007,37(3):506-512.

[16] 李忠诚.英台气田LS1区块火山岩相与储集性关系研究[J].天然气勘探与开发,2010,33(4):15-17.

Li Zhongcheng.Relationship between volcanic lithofacies and reservoir property of Longshen 1 block,Yingtai gasfield[J].Natural Gas Exploration & Development,2010,33(4):15-17.

[17] 刘万洙,黄玉龙,庞彦明,等.松辽盆地营城组中基性火山岩成岩作用:矿物晶出序列、杏仁体充填和储层效应[J].岩石学报,2010,26(1):158-164.

Liu Wanzhu,Huang Yulong,Pang Yanming,et al.Diagenesis of intermediate and mafic volcanic rocks of Yingcheng Formation(K₁y) in the Songliao basin:Sequential crystallization,amygdule filling and reservoir effect[J].Acta Petrologica Sinica,2010,26(1):158-164.

[18] 《地球科学大辞典》编辑委员会.地球科学大辞典:应用学科卷[M].北京:地质出版社,2005:388.

"A dictionary of earth sciences" Editorial Committee.A dictionary of earth sciences :application of the subject volume[M].Beijing:Geological Publishing House,2005:388.

[19] 柳广弟,张厚福.石油地质学[M].第四版.北京:石油工业出版社,2009:34.

Liu Guangdi,Zhang Houfu.Petroleum geology[M].4th ed.Beijing:Petroleum Industry Press,2009:34.

[20] 刘小洪,罗静兰,张三,等.榆林-神木地区上古生界盒8段及山2段气层的成岩作用和成岩相[J].石油与天然气地质,2006,27(2):200-209.

Liu Xiaohong,Luo Jinglan,Zhang Shan,et al.Diagenesis and diageneic facies of gas reservoirs in the upper Paleozoic 8th member of Shihezi Fm.and 2nd member of Shanxi Fm.in Yulin-Shenmu area,Ordos basin[J].Oil & Gas Geology,2006,27(2):200-209.

[21] 李阳.惠民凹陷基山砂体成岩作用及对油气圈闭的影响[J].岩石学报,2006,22(8):2205-2212.

Li Yang.Sandstone diagenesis and its influences on hydrocarbon traps in Jishan sand-body in Huimin depression,north China[J].Acta Petrologica Sinica,2006,22(8):2205-2212.

[22] 陈丽华.任丘油田震旦亚界雾迷山组碳酸盐岩微孔隙的扫描电镜观察[J].石油学报,1982,1(1):19-22.

Chen Lihua.Micro-pores in carbonate rocks of sub-sinian Wumishan Formation of Renqiu oil field under scanning electron microscopic observation[J].Acta Petrolei Sinica,1982,1(1):19-22.

[23] Worden R H,Morad S.clay minerals in sandstones:controls on formation,distribution and evolution[J].Int.Assoc.Sedimentol.Spec.Publ.2003,34:3-41.

[24] Hurst A,Nadeau P H.Clay microporosity in reservoir sandstones:an application of quantitative electron microscopy in petrophysical evaluation[J].AAPG Bulletin,1995,79(4):563-573.

[25] 赵海玲,王成,刘振文,等.火山岩储层斜长石选择性溶蚀的岩石学特征和热力学条件[J].地质通报,2009,28(4):412-419.

Zhao Hailing,Wang Cheng,Liu Zhenwen,et al.Characteristics of petrology and thermodynamics of selective dissolution of plagioclase in volcanic reservoir rocks[J].Geological Bulletin of China,2009,28(4):412-419.

松辽盆地南部英台断陷营城组火山岩晶间微孔特征及储层效应

Intercrystalline micropore characteristics and reservoir effect of Yingcheng Formation volcanic rock in Yingtai fault depression, southern Songliao Basin

PDF

可视化

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	王杰青, 许淑梅, 任新成, 池鑫琪, 舒鹏程, 刘弦, 孔家豪. 准噶尔盆地腹部西侧侏罗系三工河组储层成岩作用及控制因素[J]. 石油学报, 2021, 42(3): 319-331.
[2]	庞小军, 牛成民, 杜晓峰, 王清斌, 代黎明. 渤海海域石臼坨凸起东北缘沙河街组一段+二段砂砾岩储层差异定量表征[J]. 石油学报, 2020, 41(9): 1073-1088.
[3]	邓铭哲, 方成名, 邓棚, 张永, 朱建峰. 松辽盆地南部梨树地区走滑-逆冲构造的成因——以小宽断裂带为例[J]. 石油学报, 2020, 41(9): 1089-1099.
[4]	唐华风, 戴岩林, 郭天婵, 刘钊, 何贤培, 张一弛. 侵出式火山机构储层的分布模式——以伊通火山群为例[J]. 石油学报, 2020, 41(7): 809-820.
[5]	王彤, 朱筱敏, 张自力, 刘宇, 郭诚, 李卓. 莱州湾凹陷北洼沙河街组三段砂岩储层孔隙定量演化模式[J]. 石油学报, 2020, 41(6): 671-690.
[6]	曾联波, 刘国平, 朱如凯, 高志勇, 巩磊, 吕文雅. 库车前陆盆地深层致密砂岩储层构造成岩强度的定量评价方法[J]. 石油学报, 2020, 41(12): 1601-1609.
[7]	唐华风, 王璞珺, 边伟华, 黄玉龙, 高有峰, 代晓娟. 火山岩储层地质研究回顾[J]. 石油学报, 2020, 41(12): 1744-1773.
[8]	孙立东, 陆加敏, 杨步增, 刘家军, 李晶, 张莹, 戴世立, 徐妍, 蔡东梅. 松辽盆地北部中央古隆起带天然气成藏条件与勘探方向[J]. 石油学报, 2020, 41(10): 1163-1173.
[9]	张荣虎, 曾庆鲁, 王珂, 王俊鹏, 孟广仁, 李娴静. 储层构造动力成岩作用理论技术新进展与超深层油气勘探地质意义[J]. 石油学报, 2020, 41(10): 1278-1292.
[10]	傅宁, 王柯, 贾庆军. “源热共控”北部湾盆地福山凹陷油气的形成[J]. 石油学报, 2019, 40(S2): 38-45.
[11]	王家豪, 彭光荣, 柳保军, 郑金云, 杨飞. 碎屑岩成岩拉平处理及沉积作用控制储层物性的定量表征——以珠江口盆地白云凹陷为例[J]. 石油学报, 2019, 40(s1): 115-123.
[12]	高凤琳, 宋岩, 梁志凯, 李卓, 原园, 张瀛涵, 陈磊, 郭望. 陆相页岩有机质孔隙发育特征及成因——以松辽盆地长岭断陷沙河子组页岩为例[J]. 石油学报, 2019, 40(9): 1030-1044.
[13]	王永卓, 周学民, 印长海, 舒萍, 曹宝军, 朱映康. 徐深气田成藏条件及勘探开发关键技术[J]. 石油学报, 2019, 40(7): 866-886.
[14]	张莉, 王威, 舒志国, 郝芳, 邹华耀, 杨烁. 川东北元坝地区须家河组钙质交代—胶结致密层分布与成因[J]. 石油学报, 2019, 40(6): 692-705.
[15]	杨笑, 王志章, 周子勇, 魏周城, 曲康, 王翔宇, 王如意. 基于参数优化AdaBoost算法的酸性火山岩岩性分类[J]. 石油学报, 2019, 40(4): 457-467.