Please use this identifier to cite or link to this item: https://hdl.handle.net/11499/37192
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dc.contributor.authorAltınoğlu, Fatma Figen-
dc.date.accessioned2021-02-02T09:24:26Z
dc.date.available2021-02-02T09:24:26Z
dc.date.issued2020-
dc.identifier.issn1866-7511-
dc.identifier.urihttps://hdl.handle.net/11499/37192-
dc.identifier.urihttps://doi.org/10.1007/s12517-020-05294-x-
dc.description.abstractDetection of the linear features is a useful task to understand the tectonism of a region. Gravity anomaly data was used to investigate the tectonic structures of SE part of Denizli, western Anatolia. This region is a tectonically active transition zone between Aegean extensional and Anatolian Taurides compressional provinces. Lineaments are appearance of the instantaneous change in the density of the subsurface rocks in gravity data. To determine the lineaments, derivative-based edge detection methods, horizontal gradient, analytic signal, tilt angle and hyperbolic tilt angle applied gravity anomaly data. In defining the lineaments, 3D sediment-basement model, elevation, geology and seismicity data were used comparatively. The sediment-basement topography was modelled by 3D inversion of gravity data. The maximum sediment thickness is defined 2.4 km in the northern part of Acıpayam basin and 2.3 km in the southern part of Denizli basin. The earthquake distribution map, geology and elevation maps were provided insight the linear features of the region. As a result of the study, the new tectonic map is attained. Besides the known structures, many new lineaments and some buried faults were defined in the study area. © 2020, Saudi Society for Geosciences.en_US
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.relation.ispartofArabian Journal of Geosciencesen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectEdge detectionen_US
dc.subjectGravityen_US
dc.subjectLineamenten_US
dc.subjectWestern Anatoliaen_US
dc.subjectdetection methoden_US
dc.subjectextensional tectonicsen_US
dc.subjectgravity anomalyen_US
dc.subjectlineamenten_US
dc.subjecttectonic structureen_US
dc.subjecttilten_US
dc.subjecttransition zoneen_US
dc.subjectDenizli [Turkey]en_US
dc.subjectTurkeyen_US
dc.titleStructural interpretation of SW part of Denizli, Turkey, based on gravity data analysisen_US
dc.typeArticleen_US
dc.identifier.volume13en_US
dc.identifier.issue8en_US
dc.identifier.doi10.1007/s12517-020-05294-x-
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.identifier.scopus2-s2.0-85083549838en_US
dc.identifier.wosWOS:000526456100001en_US
dc.identifier.scopusqualityQ2-
dc.ownerPamukkale University-
item.openairetypeArticle-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextNo Fulltext-
item.grantfulltextnone-
item.cerifentitytypePublications-
crisitem.author.dept10.08. Geological Engineering-
Appears in Collections:Mühendislik Fakültesi Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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