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基于三参数小波的频谱分解方法
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  • 英文篇名:Spectrum decomposition based on three-parameter wavelet
  • 作者:朱振宇 ; 高佳伦 ; 姜秀娣 ; 孙文博 ; 薛东川 ; 王清振
  • 英文作者:Zhu Zhenyu;Gao Jialun;Jiang Xiudi;Sun Wenbo;Xue Dongchuan;Wang Qingzhen;CNOOC Research Institute;China University of Petroleum (Beijing);
  • 关键词:谱分解 ; 三参数小波 ; 小波变换 ; 时频分析 ; 储层预测
  • 英文关键词:spectrum decomposition;;three-parameter wavelet;;wavelet transform;;time-frequency analysis;;reservoir characterization
  • 中文刊名:SYDQ
  • 英文刊名:Oil Geophysical Prospecting
  • 机构:中海油研究总院有限责任公司;中国石油大学(北京);
  • 出版日期:2018-12-15
  • 出版单位:石油地球物理勘探
  • 年:2018
  • 期:v.53
  • 基金:国家重点研发计划课题“南海多类型天然气水合物成藏地质过程与富集规律(2017YFC0307301)”;; 中海石油(中国)有限公司科技项目“珠江口盆地时移地震技术应用先导研究”(YXKY-2017-ZY-14)联合资助
  • 语种:中文;
  • 页:SYDQ201806023
  • 页数:9
  • CN:06
  • ISSN:13-1095/TE
  • 分类号:18+201-208
摘要
首先阐述了频谱分解方法的基本原理,然后介绍了三参数小波,重点研究了每个参数对小波的影响,随后设计了正演模型,利用三参数小波进行时频分析;最后利用基于三参数小波的频谱分解方法预测储层,发现三参数小波能更好地显示细微的地质信息。模型测试及实际地震资料应用表明:①三参数小波的灵活性高,小波的调制频率σ影响小波的震荡程度。能量衰减因子τ影响小波的宽窄,当τ较大时,σ对小波的影响减弱。能量延迟因子β的影响颇为复杂,当其为周期的整数倍时,小波只产生时移,可以匹配零相位子波;当其为周期的非整数倍时,小波不仅产生时移,而且产生相位延迟,可以匹配非零相位子波。同时需要注意,β非零会造成河道埋深解释错误。②三参数小波变换较Morlet小波变换具有较好的时频分辨率,能更好地刻画薄互层内细微的地质沉积结构。③实际处理中可将从目的层段提取的地震子波与三参数小波做相关,优选相关性大的参数组合,从而获得最佳的三参数小波。
        We first describe the basic principle of spec-trum decomposition,then introduce three-parameter wavelet,study the influence of each parameter on wavelet.After that we conduct time-frequency analysis with three parameters based on forward modeling.Finally we perform reservoir characterization with three-parameter wavelet.It is found that subtle geological information can be highlighted.The following understanding are obtained based on model and real data tests:①The three-parameter wavelet has high flexibility,the modulation frequencyσof the wavelet affects the vibration degree of the wavelet,the energy attenuation parameterτcontrols attenuation speed of attenuation function.When the value ofτis relatively big,theσhas less influence on the wavelet.The influence of the energy lag parameterβon the wavelet shape is more complex.Whenβis an integer multiple of trigonometric function period,only wavelet time shift occurs,it can be used to match the zero phase wavelet;when theβis not an integer multiple of trigonometric function period,wavelet time shift and deformation are generated,it can be used to match the non-zero phase wavelet.Deeply buried channels may be misinterpreted whenβis not equal to zero;②Compared with Morlet wavelet,three-parameter wavelet can more precisely depict subtle sedimentary structures in thin interbeds;③In real data processing,the optimal parameter combinations can be obtained according to the correlation of various forms of basic wavelets with real wavelet extracted from targets.
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