Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol S (Solid Earth Sciences) » S-EM Earth's Electromagnetism

[S-EM36_30PM2] Electrical conductivity, Tectono-electromagnetism

Wed. Apr 30, 2014 4:15 PM - 5:45 PM 413 (4F)

Convener:*Ken'ichi Yamazaki(Disaster Prevention Research Institute, Kyoto University), Noriko Tada(Japan Agency for Marine-Earth Science and Technology), Chair:Noriko Tada(Japan Agency for Marine-Earth Science and Technology), Ken'ichi Yamazaki(Disaster Prevention Research Institute, Kyoto University)

5:00 PM - 5:15 PM

[SEM36-06] Robust magnetotelluric inversion

*Tetsuo MATSUNO1, Alan CHAVE2, Alan JONES3, Mark MULLER3, Rob EVANS2 (1.National Institute of Polar Research, 2.Woods Hole Oceanographic Institution, 3.Dublin Institute for Advanced Studies)

Keywords: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.