薛诗桂, 郝守玲. 入射频率对煤系薄互层地震响应特征影响的物理模拟[J]. 煤田地质与勘探, 2014, 42(5): 92-95. DOI: 10.3969/j.issn.1001-1986.2014.05.018
引用本文: 薛诗桂, 郝守玲. 入射频率对煤系薄互层地震响应特征影响的物理模拟[J]. 煤田地质与勘探, 2014, 42(5): 92-95. DOI: 10.3969/j.issn.1001-1986.2014.05.018
XUE Shigui, HAO Shouling. Physical simulation for the influence of incident frequency on seismic response characteristic of thin alternating layers in coal measures[J]. COAL GEOLOGY & EXPLORATION, 2014, 42(5): 92-95. DOI: 10.3969/j.issn.1001-1986.2014.05.018
Citation: XUE Shigui, HAO Shouling. Physical simulation for the influence of incident frequency on seismic response characteristic of thin alternating layers in coal measures[J]. COAL GEOLOGY & EXPLORATION, 2014, 42(5): 92-95. DOI: 10.3969/j.issn.1001-1986.2014.05.018

入射频率对煤系薄互层地震响应特征影响的物理模拟

Physical simulation for the influence of incident frequency on seismic response characteristic of thin alternating layers in coal measures

  • 摘要: 建立薄互层地震物理模型,分别从低频和高频入射时地震记录的振幅谱形态、振幅、频率特征、AVO特征等方面入手,分析了入射频率对煤系薄互层模型地震响应特征的影响。结果表明:入射频率对薄互层层数变化反映敏感,高频入射时振幅谱形态可分辨的厚度比较小,分辨率较高;振幅谱幅值以及主频值的变化与薄互层的总厚度和波长之比有关,并且随着厚度的增加其变化规律符合薄层的振幅调谐规律与频率调谐规律;入射频率不同时,AVO曲线特征也不相同,在进行薄互层资料的对比解释及AVO分析时,要充分考虑入射频率所引起的差异。

     

    Abstract: Using seismic physical model and from the spectrum patterns, amplitude, frequency and AVO characteristics of seismic records of low and high incident frequency, the paper analyzed the influence of incident frequency on seismic response characteristics for thin alternating layers in coal measures. It shows that the incident frequency is sensitive to the variation of the number of alternating layers, the amplitude and spectrum patterns of high frequency incidence can resolve small thickness and have higher resolution, the amplitude spectrum and frequency values are related to the ratio of the thickness of a thin alternating layer and wavelength, and with the increase of the thickness, its variation rule is in accordance with the tuning rule of the amplitude and frequency. For different incident frequency, the AVO curve characteristics are different. In seismic interpretation and AVO analysis of thin alternating layers, we should fully consider the differences caused by the incident frequency.

     

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