Publication:
Use of ssq rotational invariant of magnetotelluric impedances for estimating informative properties for galvanic distortion 1. Geomagnetism

dc.contributor.authorT. Rung-Arunwanen_US
dc.contributor.authorW. Siripunvarapornen_US
dc.contributor.authorH. Utadaen_US
dc.contributor.otherMahidol Universityen_US
dc.contributor.otherCommission on Higher Educationen_US
dc.contributor.otherUniversity of Tokyoen_US
dc.contributor.otherCurl-E Geophysics Co. Ltd.en_US
dc.date.accessioned2018-12-21T07:26:54Z
dc.date.accessioned2019-03-14T08:03:32Z
dc.date.available2018-12-21T07:26:54Z
dc.date.available2019-03-14T08:03:32Z
dc.date.issued2017-12-01en_US
dc.description.abstract© 2017 The Author(s). Several useful properties and parameters - a model of the regional mean one-dimensional (1D) conductivity profile, local and regional distortion indicators, and apparent gains - were defined in our recent paper using two rotational invariants (det: determinant and ssq: sum of squared elements) from a set of magnetotelluric (MT) data obtained by an array of observation sites. In this paper, we demonstrate their characteristics and benefits through synthetic examples using 1D and three-dimensional (3D) models. First, a model of the regional mean 1D conductivity profile is obtained using the average ssq impedance with different levels of galvanic distortion. In contrast to the Berdichevsky average using the average det impedance, the average ssq impedance is shown to yield a reliable estimate of the model of the regional mean 1D conductivity profile, even when severe galvanic distortion is contained in the data. Second, the local and regional distortion indicators were found to indicate the galvanic distortion as expressed by the splitting and shear parameters and to quantify their strengths in individual MT data and in the dataset as a whole. Third, the apparent gain was also shown to be a good approximation of the site gain, which is generally claimed to be undeterminable without external information. The model of the regional mean 1D profile could be used as an initial or a priori model in higher-dimensional inversions. The local and regional distortion indicators and apparent gains could be used to examine the existence and to guess the strength of the galvanic distortion. Although these conclusions were derived from synthetic tests using the Groom-Bailey distortion model, additional tests with different distortion models indicated that these conclusions are not strongly dependent on the choice of distortion model. These galvanic-distortion-related parameters would also assist in judging if a proper treatment is needed for the galvanic distortion when an MT dataset is given. Hence, this information derived from the dataset would be useful in MT data analysis and inversion. [Figure not available: see fulltext].en_US
dc.identifier.citationEarth, Planets and Space. Vol.69, No.1 (2017)en_US
dc.identifier.doi10.1186/s40623-017-0665-8en_US
dc.identifier.issn18805981en_US
dc.identifier.issn13438832en_US
dc.identifier.other2-s2.0-85020505324en_US
dc.identifier.urihttps://repository.li.mahidol.ac.th/handle/20.500.14594/42488
dc.rightsMahidol Universityen_US
dc.rights.holderSCOPUSen_US
dc.source.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85020505324&origin=inwarden_US
dc.subjectEarth and Planetary Sciencesen_US
dc.titleUse of ssq rotational invariant of magnetotelluric impedances for estimating informative properties for galvanic distortion 1. Geomagnetismen_US
dc.typeArticleen_US
dspace.entity.typePublication
mu.datasource.scopushttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85020505324&origin=inwarden_US

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