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探测一阶模态三重分裂的MSE技术和SHS方法的比较研究

DOI: 10.6038/cjg20131008, PP. 3313-3323

Keywords: 多台站实验技术,球谐叠加法,模态剥离,3S1,异常分裂

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Abstract:

完全剥离一阶模态nS1的三重分裂信号将有助于识别出其全部分裂谱线,进而更好地约束地球内部结构.理想情况下,球谐叠加法(SHS)与多台站实验技术(MSE)均可剥离一阶模态nS1的三重分裂信号,但部分学者持不同观点.本文基于对二者的理论分析进一步确认,在自耦合前提下,MSE方法可成功剥离nS1的三重分裂信号;而SHS方法在实际应用中无法成功剥离nS1的三重分裂信号,但可相对增强目标信号的振幅强度.此外,本文解释了MSE可剥离单线态信号的真实原因,并指出由于MSE未考虑全频段耦合影响,故仅适用于1mHz以下的低频模态.鉴于超导重力(SG)数据在1mHz以下比宽频地震数据具有更高的信噪比,因此,为验证本文结论并弄清MSE和SHS的实质,基于模拟数据及SG台站实测数据,本文利用MSE和SHS分别对一阶模态的合成信号及模态3S1进行了探测分析.实验结果表明,MSE可成功剥离一阶模态三重分裂信号,SHS则无法完全剥离,验证了我们的理论结论,表明前人部分结果需重新审视与评价.此外,本文基于三种不同方法并利用13个SG台站数据给出的3S1的分裂宽度比分别为1.008,1.000和1.001,远小于异常分裂判别临界值1.5,因此,3S1应是正常分裂模态.

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