松辽盆地南部火山岩储层主控因素
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摘要
松辽盆地南部火山岩储层是由孔、缝、洞构成的多孔介质储层,其储集空间类型多样、结构复杂,储层物性在空间上变化大,非均质性强,相变快。在勘探过程中需要解决的首要问题就是弄清楚火山岩储层形成的主要控制因素。通过地质、测井和地震资料,结合现有勘探成果,分析发现松南地区火山岩储层发育的三级控制规律:①火山机构类型控制储层发育程度,流纹质火山机构储层物性最好;②火山机构-相带控制储层展布,火山口-近火山口相带物性最好;③成岩作用和构造裂缝控制储层有效性,隐爆角砾岩化作用、风化淋滤作用以及裂缝使储层物性变好。清楚认识火山岩储层发育的控制因素,对储层预测及今后气田的有效开发具有重要意义。
Volcanic reservoirs in the southern Songliao Basin are characterized by various types of accumulation space and complex structures,they are porous reservoirs composed of different media,including different pores,fractures and holes,and their physical properties vary greatly in space,with strong heterogeneity and changeful facies.The most important issue that needs to be solved in exploration is to make main controlling factors for the formation of volcanic reservoirs clear.Combined geological,logging and seismic data with current exploration results,we proposed a three-grade rule that controls the development of volcanic reservoirs in the southern Songliao Basin.①Types of the volcanic edifice control the development degree of reservoirs and a reservoir with the rhyolitic volcanic edifice has the best physical property.②A volcanic edifice-facies belt controls the distribution of reservoirs and a crater-near crater facies(CNCF) belt shows the best physical property.③Diagenesis and tectoclase jointly control the effectiveness of reservoirs,and the cryptoexplosion brecciation and weathering-leaching coupled with fractures bring about a better physical property.The different volcanic edifice has different pore spaces and physical properties of reservoirs.It is significance in predicting reservoirs and effectively exploiting gas accumulations to clearly recognize controlling factors for the development of volcanic reservoirs.
引文
[1]Wang P J,Liu W Z,Wang S X,et al.40Ar/39Ar and K/Ar datingon the volcanic rocks in the Songliao basin,NE China:Con-straints on stratigraphy and basin dynamics[J].InternationalJournal of Earth Sciences,2002,91:331-340.
    [2]Wang P J,Ren Y G,Shan X L,et al.The Cretaceous volcanicsuccession around the Songliao Basin,NE China:Relationshipbetween volcanism and sedimentation[J].Geological Journal,2002,37(2):97-115.
    [3]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.Discussion on the forma-tion mechanism of volcanic oil and gas reservoirs[J].Acta Petro-logica Sinica,2010,26(1):1-13.
    [4]冯志强,刘嘉麒,王璞珺,等.油气勘探新领域:火山岩油气藏——松辽盆地大型火山岩气田发现的启示[J].地球物理学报,2011,54(2):269-279.Feng Zhiqiang,Liu Jiaqi,Wang Pujun,et al.New oil and gas ex-ploration field:Volcanic hydrocarbon reservoirs—Enlightenmentfrom the discovery of the large gas field in Songliao Basin[J].Chinese J.Geophys.,2011,54(2):269-279.
    [5]侯启军.南北辉映,气贯松辽——吉林油田公司长岭断陷长深1井发现纪略[J].中国石油企业,2006,(3):45-46.Hou Qijun.Gas through out the Songliao Basin:Discovery ofWell CS1in Changling fault depression of Jilin Oilfeild company[J].China Petroleum Enterprise,2006,(3):45-46.
    [6]黄薇,邵红梅,赵海玲,等.松辽盆地北部徐深气田营城组火山岩储层特征[J].石油学报,2006,27(S1):47-51.Huang Wei,Shao Hongmei,Zhao Hailing,et al.Characteristics ofYingcheng Formation's volcanic reservoir in Xushen Gas Field innorthern Songliao Basin[J].Acta Petrolei Sinica,2006,27(S1):47-51.
    [7]王璞珺,庞颜明,唐华风,等.松辽盆地白垩系营城组古火山机构特征[J].吉林大学学报:地球科学版,2007,37(6):1064-1073.Wang Pujun,Pang Yanming,Tang Huafeng,et al.The character-istics of the paleo-volcanic edifice of Yingcheng Formation,Cre-taceous,Songliao Basin[J].Journal of Jilin University:Earth Sci-ence Edition,2007,37(6):1064-1073.
    [8]唐华风,庞颜明,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):841-852.Tang Huafeng,Pang Yanming,Bian Weihua,et al.Quantitativeanalysis on reservoirs in volcanic edifice of Early CretaceousYingcheng Formation in Songliao Basin[J].Acta Petrolei Sinica,2008,29(6):841-852.
    [9]侯启军,赵志魁,王立武,等.松辽盆地深层天然气富集条件的特殊性[J].大庆石油学院学报,2009,33(2):31-35.Hou Qijun,Zhao Zhikui,Wang Liwu,et al.Discussion of the particu-larity of deep natural gas enrichment conditions in Songliao Basin[J].Journal of Daqing Petroleum Institute,2009,33(2):31-35.
    [10]蔡周荣,夏斌,郭峰,等.松辽盆地北部徐家围子断陷营城组火山岩受控机制分析[J].石油学报,2010,31(6):440-444.Cai Zhourong,Xia Bin,Guo Feng,et al.Controlling mechanismon volcanic rocks of the Yingcheng Formation of the Xujiaweizirift depression in the northern Songliao Basin[J].Acta PetroleiSinica,2010,31(6):440-444.
    [11]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 charac-teristics and evolution of volcanic rocks in Xujiaweizi fault de-pression[J].Acta Petrolei Sinica,2010,31(3):400-407.
    [12]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 ofthe Songliao Basin:Classification,characteristics and reservoirSignificance[J].Journal of Jilin University:Earth Science Edi-tion,2003,33(4):449-456.
    [13]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 ofthe Songliao Basin:Sequence,model and the quantitative relationshipwith porosity&permeability of the volcanic reservoir[J].Journal ofJilin University:Earth Science Edition,2006,36(5):805-812.
    [14]边伟华,陈玉魁,唐华风,等.火山岩相的岩屑识别—以松辽盆地南部东岭探区为例[J].吉林大学学报:地球科学版,2007,37(6):1104-1109.Bian Weihua,Chen Yukui,Tang Huafeng,et al.Volcanic facies i-dentification with cuttings:A case study in Dongling,SouthernSongliao Basin[J].Journal of Jilin University:Earth Science Edi-tion,2007,37(6):1104-1109.
    [15]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):1252-1258.Gao Youfeng,Liu Wanzhu,Ji Xueyan,et al.Diagenesis types andfeatures of volcanic rocks and its impact on porosity and permea-bility in Yingcheng Formation,Songliao Basin[J].Journal of JilinUniversity:Earth Science Edition,2007,37(6):1252-1258.
    [16]王璞珺,郑常青,舒萍,等.松辽盆地深层火山岩岩性分类方案[J].大庆石油地质与开发,2007,26(4):17-22.Wang Pujun,Zheng Changqing,Shu Ping,et al.Classification ofdeep volcanic rocks in Songliao Basin[J].Petroleum Geology&Oilfield Development in Daqing,2007,26(4):17-22.
    [17]庞彦明,章凤奇,邱红枫,等.酸性火山岩储层微观孔隙结构及物性参数特征[J].石油学报,2007,28(6):72-77.Pang Yanming,Zhang Fengqi,Qiu Hongfeng,et al.Characteristics ofmicroscopic pore structure and physical property parameter in acidicvolcanic reservoir[J].Acta Petrolei Sinica,2007,28(6):72-77.
    [18]吴颜雄,王璞珺,宋立忠,等.松辽盆地营城组火山机构相带地震-地质解译[J].地球物理学报,2011,54(1):545-555.Wu Yanxiong,Wang Pujun,Song Lizhong,et al.Seismic volcanos-tratigraphy of Yingcheng Formation in the Songliao Basin,Creta-ceous,NE China[J].Chinese J.Geophys.,2011,54(1):545-555.
    [19]李喆,王璞珺,纪学雁,等.松辽盆地东南隆起区营城组火山岩相和储层的空间展布特征[J].吉林大学学报:地球科学版,2007,37(6):1224-1231.Li Zhe,Wang Pujun,Ji Xueyan,et al.The spatial distribution ofvolcanic facies and reservoir in Yingcheng Formation of SouthUplifted Area of Songliao Basin[J].Journal of Jilin University:Earth Science Edition,2007,37(6):1224-1231.
    [20]Schmincke H U.Volcanism[M].Berlin,Heidelberg,New York:Springer,2004.

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