日本地球惑星科学連合2014年大会

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セッション記号 S (固体地球科学) » S-EM 固体地球電磁気学

[S-EM36_30PM2] 電気伝導度・地殻活動電磁気学

2014年4月30日(水) 16:15 〜 17:45 413 (4F)

コンビーナ:*山崎 健一(京都大学防災研究所)、多田 訓子(海洋研究開発機構)、座長:多田 訓子(海洋研究開発機構)、山崎 健一(京都大学防災研究所)

17:00 〜 17:15

[SEM36-06] 統計学的に頑健なMTインバージョン

*松野 哲男1Chave Alan2Jones Alan3Muller Mark3Evans Rob2 (1.国立極地研究所、2.ウッズホール海洋研究所、3.ダブリン高等研究所)

キーワード:Inversion, Probability distribution, Magnetotellurics

A robust magnetotelluric (MT) inversion algorithm has been developed on the basis of quantile-quantile (q-q) plotting with confidence band and statistical modelling of inversion residuals for the MT response function (apparent resistivity and phase). Once outliers in the inversion residuals are detected in the q-q plot with the confidence band and the statistical modelling with the Akaike information criterion, they are excluded from the inversion data set and a subsequent inversion is implemented with the culled data set. The exclusion of outliers and the subsequent inversion is repeated until the q-q plot is substantially linear within the confidence band, outliers predicted by the statistical modelling are unchanged from the prior inversion, and the misfit statistic is unchanged at a target level. The robust inversion algorithm was applied to synthetic data generated from a simple 2-D model and observational data from a 2-D transect in southern Africa. Outliers in the synthetic data, which come from extreme values added to the synthetic responses, produced spurious features in inversion models, but were detected by the robust algorithm and excluded to retrieve the true model. An application of the robust inversion algorithm to the field data demonstrates that the method is useful for data clean-up of outliers, which could include model as well as data inconsistency (for example, inability to fit a 2-D model to a 3-D data set), during inversion and for objectively obtaining a robust and optimal model. The present statistical method is available irrespective of the dimensionality of target structures (hence 2-D and 3-D structures) and of isotropy or anisotropy, and can operate as an external process to any inversion algorithm without modifications to the inversion program.