{"title":"2-D Interpretation of Minamikayabe MT Data Set by the Controlled Random Search Technique","authors":"V. Červ, J. Pek","doi":"10.5636/JGG.49.1717","DOIUrl":null,"url":null,"abstract":"Within the MT-DIW3 project of the comparison of various MT interpretation techniques, the controlled random search procedure was applied to the 2-D interpretation of the MT data from the Minamikayabe MT polygon in Japan. Three NE-SW profiles together with one perpendicular profile were 2-D modelled, simultaneously for both polarizations of the MT field. Although the 2-D approximation seems to be rather far from the real resistivity conditions, we could obtain relatively consistent interpretation results particularly for data within the short period range, up to 1 s. Better fit was achieved for apparent resistivities than for phases. For all NE-SW profiles, a near-surface conductive body is indicated below the central part of the polygon. At both sides of this body two deeper conductive zones are obvious. As for the perpendicular profile kb*s06, a large conductive zone is required below the SE margin of the profile.","PeriodicalId":156587,"journal":{"name":"Journal of geomagnetism and geoelectricity","volume":"03 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1997-11-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of geomagnetism and geoelectricity","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5636/JGG.49.1717","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
Within the MT-DIW3 project of the comparison of various MT interpretation techniques, the controlled random search procedure was applied to the 2-D interpretation of the MT data from the Minamikayabe MT polygon in Japan. Three NE-SW profiles together with one perpendicular profile were 2-D modelled, simultaneously for both polarizations of the MT field. Although the 2-D approximation seems to be rather far from the real resistivity conditions, we could obtain relatively consistent interpretation results particularly for data within the short period range, up to 1 s. Better fit was achieved for apparent resistivities than for phases. For all NE-SW profiles, a near-surface conductive body is indicated below the central part of the polygon. At both sides of this body two deeper conductive zones are obvious. As for the perpendicular profile kb*s06, a large conductive zone is required below the SE margin of the profile.