基于时频分析的高分辨率层序地层

吴淑玉, 刘俊. 基于时频分析的高分辨率层序地层[J]. 海洋地质与第四纪地质, 2015, 35(4): 197-207. doi: 10.16562/j.cnki.0256-1492.2015.04.021
引用本文: 吴淑玉, 刘俊. 基于时频分析的高分辨率层序地层[J]. 海洋地质与第四纪地质, 2015, 35(4): 197-207. doi: 10.16562/j.cnki.0256-1492.2015.04.021
WU Shuyu, LIU Jun. HIGH RESOLUTION SEQUENCE STRATIGRAPHIC STUDY BASIC ON TIME-FREQUENCY ANALYSIS[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 197-207. doi: 10.16562/j.cnki.0256-1492.2015.04.021
Citation: WU Shuyu, LIU Jun. HIGH RESOLUTION SEQUENCE STRATIGRAPHIC STUDY BASIC ON TIME-FREQUENCY ANALYSIS[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 197-207. doi: 10.16562/j.cnki.0256-1492.2015.04.021

基于时频分析的高分辨率层序地层

  • 基金项目:

    国土资源部海洋油气资源和环境地质重点实验室基金(MRE201318、MRE201121和MRE201115),国家海洋局海底重点实验室基金(KLSG1102),中国地质调查项目(GZH200700405)资助和国土资源部公益性行业科研专项课题(201211086-09)资助

详细信息
    作者简介: 吴淑玉(1985-),女,助理研究员,主要从事地震资料解释和反演等地球物理相关工作。E-mail:hnwushuyu@163.com
  • 中图分类号: P631.4

HIGH RESOLUTION SEQUENCE STRATIGRAPHIC STUDY BASIC ON TIME-FREQUENCY ANALYSIS

  • 在层序地层学的基础上,根据沉积旋回特征,运用时频分析的方法对北黄海东部坳陷进行高分辨率层序地层研究,将某口井的测井曲线进行一维离散小波阈值去噪与主成分分析方法融合多条测井曲线,求得能够综合反映地层信息特征的第1主成分曲线。对该曲线进行一维连续小波变换,根据模极大值得到的不同尺度因子,对不同级别的层序地层进行划分,可划分出4个层序和8个准层序组单元,并对层序单元进行沉积旋回和微相分析,以沉积微相为单元并进行小波变换,得到小尺度对应的岩层组单元划分。结果表明,对测井曲线进行小波变换能对层序地层进行高分辨率划分,并且可有效地进行沉积旋回的研究。
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出版历程
收稿日期:  2014-10-15
修回日期:  2014-12-30

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