火山岩圈闭的识别方法
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摘要
松辽盆地深层营城组天然气气藏是火山岩圈闭气藏,识别火山岩圈闭可为天然气勘探提供钻探目标。因此,通过总结徐家围子断陷火山岩圈闭模式(火山岩岩性圈闭、火山岩岩相圈闭、火山岩岩性-断层圈闭)认识了火山岩地震响应特征,同时对火山岩储层进行了层位解释及火山岩岩体识别,并应用相干体、地震反演等技术识别出松辽盆地徐家围子断陷营城组火山岩圈闭,从而形成了火山岩圈闭识别方法。应用该方法在徐家围子断陷识别了营城组火山岩圈闭,并通过钻井证实了火山岩圈闭识别方法的可行性,而且具有Ⅰ、Ⅱ类地震相特征的火山岩岩性-断层圈闭气藏的识别成功率较高。
Deep-layer natural gas reservoir in Yingcheng Formation of Songliao Basin is volcanic trap.The recognition of this kind of trap can provide the drilling target of natural gas exploration.Therefore through summing up the volcanic trap models in Xujiaweizi faulted depression(volcanic lithological trap,volcanic facies trap,and volcanic lithological-fault trap),the seismic characteristics of above rock have been understood.At the same time,layer interpretation and volcanic body recognition of volcanic reservoir have been conducted.With the help of coherent body,seismic inversion and so on techniques,the volcanic trap in Yingcheng Formation of the above depression has been recognized and then a set of determining method of above rock has been established.The feasibility of this recognizing method has been proven by drilling facts afterwards and moreover the recognized success ratio of volcanic lithological-fault trap with Ⅰand Ⅱ type seismic facies characteristics are pretty higher.
引文
[1]李石,王彤.火山岩[M].北京:地质出版社,1980.
    [2]黄玉龙,王璞珺,冯志强,等.松辽盆地改造残留的古火山机构与现代火山机构的类比分析[J].吉林大学学报(地球科学版),2007,37(1):65-72.
    [3]金成志,杨双玲,舒萍,等.升平开发区火山岩储层孔隙结构特征与产能关系综合研究[J].大庆石油地质与开发,2007,26(2):38-41.
    [4]文瑞霞,于晶.火山岩储层地震特征及识别方法[A].中国地球物理学会第二十二届年会论文集[C].成都:四川科学技术出版社,2006.
    [5]刘金平,刘云武,高君,等.岩性圈闭储层描述技术及应用[J].石油地球物理勘探,2003,38(5):531-534.
    [6]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):449-455.
    [7]蒙启安,门广田,张正和.松辽盆地深层火山岩体、岩相预测方法及应用[J].大庆石油地质与开发,2001,20(3):21-24.
    [8]张玉芬,韩世勤,熊维纲.井约束条件下的地震道反演[A].罗延钟.应用地球物理学进展[C].武汉:中国地质大学出版社,1996.

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