吉林大学学报(地球科学版)

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松辽盆地断陷层系地震火山地层学研究:典型火山岩地震相与地质解释模式

衣健1,王璞珺1,李瑞磊2,赵然磊1,陈崇阳1,孙玥3   

  1. 1.吉林大学地球科学学院,长春130061;
    2.中石化东北油气分公司勘探开发研究院,长春130062;
    3.大庆油田有限责任公司海塔勘探开发指挥部,黑龙江 大庆 163000
  • 收稿日期:2013-09-14 出版日期:2014-05-26 发布日期:2014-05-26
  • 通讯作者: 王璞珺(1959-),男,教授,博士,博士生导师,主要从事盆地火山岩和油气地震勘察研究与教学, E-mail:wangpj@jlu.edu.cn
  • 作者简介:衣健(1984-),男,博士研究生,主要从事盆地火山岩储层与油气藏研究,E-mail:yijian_x@sina.com
  • 基金资助:

    国家“973”计划项目(2009CB219303)

Seismic Volcanostratigraphy of the Songliao Basin, Early Cretaceous: Typical Volcanic Seismic Facies and Geological Interpretation Pattern

Yi Jian1,Wang Pujun1,Li Ruilei2,Zhao Ranlei1,Chen Congyang1,Sun Yue3   

  1. 1.College of Earth Sciences,Jilin University,Changchun130061,China;
    2.Northeast Branch,SINOPEC,Changchun130062,China;
    3.Hailaer Retroleum Exploretion & Pevelopment Headquaters of Daqing oilfield, Daqing 163000, Heilongjiang, China
  • Received:2013-09-14 Online:2014-05-26 Published:2014-05-26

摘要:

为了研究松辽盆地火山岩盆地充填模式及在无井或少井区寻找火山岩有利储层,需要对盆地火山岩地震相及其反射特征和地质内涵进行系统性的总结和分析。基于盆内钻井和过井地震剖面,应用火山地层学理论和地震火山地层学方法将松辽盆地火山岩地震相单元划分为火山岩丘、火山岩台地、洼地火山充填、穿切等4类10种亚类。通过井震对比,结合野外火山地层研究相关文献资料,阐述了这些地震相单元的地质解释模式和响应关系。火山岩地震相单元通常对应于以某种盆地火山充填类型(相或相组合)为主的火山岩体,火山岩丘地震相多可解释为侵出岩穹、酸性简单熔岩流和酸性复合熔岩流等具有丘状外形的充填类型,火山岩台地地震相多代表中基性岩的简单熔岩流和火山碎屑流等具有席状外形的充填类型,洼地火山充填多代表充填在先存洼地中的简单熔岩流和火山碎屑流,穿切地震相多可解释为岩席、岩墙。除了这些典型的地震相单元以外,对地震反射特征(外形、物理参数、反射结构)与火山岩地质属性的响应关系的分析可有助于更好地解释地震相单元所反映的地质含义。

关键词: 松辽盆地断陷层系, 地震火山地层学, 地震相单元, 火山岩盆地充填类型, 响应关系

Abstract:

In order to understand the volcanic rocks filling model in basin and explore favorable volcanic reservoir in less or no well area, the systematically study of seismic facies units, their reflection characteristics and geological interpretation is necessary. With volcanostratigraphy theory and seismic volcanostratigraphy method, the typical seismic facies of the volcanic rocks were studied based on wells and inter-well seismic profiles in the Songliao volcanic rifted grabens, Early Cretaceous. The facies can be divided into 4 types and 10 subtypes of typical seismic facies units, such as the volcanic dome unit, the volcanic platform unit, the volcanic filling unit and the cutting units. Based on wellseismic contrast and the references of volcanostratigraphy study in the field, the geological models of seismic units and their response relationship are described. Seismic facie units usually correspond to the volcanic rocks with the main filling type (facies and facies association) composition; the volcanic dome unit can be interpreted as the domeshaped extrusion dome, the acid simple lava flow, the acid compound lava flow and so on; the volcanic platform unit can be interpreted as the platform-shaped basic-intermediate simple lava flow and the pyroclastic flow; the volcanic filling unit can be interpreted as the simple lave flow and volcanic pyroclastic flow which fill in the preceding low-lying land;the cutting units can be interpreted as the sheet, dike. Besides the seismic facies, the analysis of geological attributes of seismic reflection characteristics are favorable to understand geological meaning much better.

Key words: rift sequences of Songliao basin, seismic volcanostratigraphy, seismic units, filling patterns of basin volcanic rocks, response relationship

中图分类号: 

  • P539.1
[1] 李尚林,王根厚,马伯永,杨文瑞,赵文涛,廖蕾. 藏北比如县玛双布上三叠统波里拉组震积事件沉积的发现及意义[J]. J4, 2008, 38(6): 973-0979.
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