Edge Detection Analysis Using EMAG2 Magnetic Data in Lake Van and Its Surroundings, Türkiye

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Özet

The aim of this study is to use EMAG2 magnetic data to analyze and interpret the boundaries of important structural features in and around Lake Van using various advanced edge detection techniques. The reduction pole was applied to the magnetic data. Edge detection is an important step to interpret the boundaries of geological structural elements with higher precision. A comprehensive lineament analysis was conducted by applying traditional and advanced edge-detection filtering techniques, including the Tilt angle (TA), the Tilt Angle of the Total Horizontal Gradient Amplitude (TAHG), and Total Horizontal Gradient-Based Edge Detection (THGED). With these methods, the boundaries of magnetic anomaly sources were tried to be interpreted more clearly. In these comparative results, lineations were obtained in the south of the lake and it was shown that it was affected by faults in the N-S, E-W main directions. In the north of the lake, NE-SW trending lineations were obtained.

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RDL Kalıcı Bağlantı (PID)
https://rdlopen.rawdatalibrary.net/r/gumushane/19608Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.26650/ijegeo.1643787Yayıncı resmi DOI adresi
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dc.contributor.authorAktaş, Gülten
dc.date.accessioned2026-10-22T10:52:20.023898023Z
dc.date.available2026-10-22T10:52:20.023898023Z
dc.date.issued2025
dc.description.abstractThe aim of this study is to use EMAG2 magnetic data to analyze and interpret the boundaries of important structural features in and around Lake Van using various advanced edge detection techniques. The reduction pole was applied to the magnetic data. Edge detection is an important step to interpret the boundaries of geological structural elements with higher precision. A comprehensive lineament analysis was conducted by applying traditional and advanced edge-detection filtering techniques, including the Tilt angle (TA), the Tilt Angle of the Total Horizontal Gradient Amplitude (TAHG), and Total Horizontal Gradient-Based Edge Detection (THGED). With these methods, the boundaries of magnetic anomaly sources were tried to be interpreted more clearly. In these comparative results, lineations were obtained in the south of the lake and it was shown that it was affected by faults in the N-S, E-W main directions. In the north of the lake, NE-SW trending lineations were obtained.
dc.identifier.doi10.26650/ijegeo.1643787
dc.identifier.eissn2148-9173
dc.identifier.endpage127
dc.identifier.issue2
dc.identifier.startpage119
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/19608
dc.identifier.volume12
dc.language.isoen
dc.relation.ispartofInternational Journal of Environment and Geoinformatics
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectMühendislik, Jeoloji
dc.subjectÇevre Bilimleri
dc.subjectMineraloji
dc.titleEdge Detection Analysis Using EMAG2 Magnetic Data in Lake Van and Its Surroundings, Türkiye
dc.typeArticle
dspace.entity.typePublication
rdl.citation.openalex1
rdl.citation.trdizin1
rdl.oa.statusgold
rdl.oa.urlhttps://doi.org/10.26650/ijegeo.1643787
rdl.source.indexTRDIZIN