Finally, variance analysis is used to verify the validity of the crytic model.

后，利用方差分析周期检验方法作了印证性讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学的差分能量法,对高邮台电阻率日均值进行处理分析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波的相关理论,采用时域有限差分法建立浅海沉积层中界面波传播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利用方差析验方法作了印证讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学的差能量法,对高邮台电阻率日均值进行处理析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波的相关理论,采用时域有限差法建立浅海沉积层中界面波传播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利用方析周期检验方法作了印证性讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学的能量法,对高电阻率日均值进行处理析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波的相关理论,采用时域有法建立浅海沉积层中界面波传播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利用方周期检验方法作了印证性讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学的能量法,对高邮台电阻率日值进行处理。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波的相关理论,采用时域有限法建立浅海沉积层中界面波传播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利方差分析周期检验方法作了印证性讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

电学的差分能量法,对高邮台电阻率日均值进行处理分析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界的相关理论,采时域有限差分法建立浅海沉积层中界播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利方差分析周期检验方法作了印证性讨。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

电学的差分能量法,对高邮台电阻率日均值进行处理分析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面的相关理,采时域有限差分法建立浅海沉积层中界面模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利用方析周期检验方法作了印证性讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学能量法,对高邮台电阻率日均值进行处理析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波相关理论,采用时域有限法建立浅海中界面波传播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利用差分析周期检法作了印证性讨论。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学的差分能量法,对高邮台电阻率日均值进行处理分析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波的相关理论,采用时域有限差分法建立浅海沉积层中界面波传播模型。

Finally, variance analysis is used to verify the validity of the crytic model.

最后，利用方差分析周期检验方法作了印证性讨。

The daily mean of the ground resistivity of Gaoyou station is processed by the method of differential energy of geoelectricity.

应用电学的差分能量法,对高邮台电阻率日均处分析。

In the framework of Geoacoustics interface wave theory,a time domain finite difference model for the propagation of interface wave in shallow sea has been developed.

根据声界面波的相,采用时域有限差分法建立浅海沉积层中界面波传播模型。