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dc.contributor.authorBilim, Funda
dc.contributor.authorAkay, Tugce
dc.contributor.authorAydemir, Attila
dc.contributor.authorKosaroglu, Sinan
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T09:45:58Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T09:45:58Z
dc.date.issued2016
dc.identifier.issn0375-6505
dc.identifier.issn1879-3576
dc.identifier.urihttps://dx.doi.org/10.1016/j.geothermics.2015.12.002
dc.identifier.urihttps://hdl.handle.net/20.500.12418/7436
dc.descriptionWOS: 000370099900004en_US
dc.description.abstractIn this study, the Curie point depth (CPD), heat-flow and radiogenic heat production maps of the Menderes Massif (MM) and the Aegean Region-Turkey were prepared for the thermal crustal structure from the aeromagnetic data by means of a spectral analysis method. The estimated CPDs in the study area vary from 6.21 to 12.41 km. The heat-flow values were calculated for two (2) different thermal conductivities of 2.5-2.7 Wm(-1) K-1. The radiogenic heat production was also calculated between 0.38 and 0.80 mu W m(-3) on the high-grade metamorphic units of the study area. The estimated heat-flow and radiogenic heat production maps indicate that a high temperature in the upper crust and thin lithosphere in the observation area are probably resulted from the crustal extension, active deformation and magmatism. All of the produced maps in this study were correlated with the analytic signal (AS) map which indicates the locations of the bodies causing magnetic anomalies. In addition, maxspots of the horizontal gradients from the magnetic anomalies were also emplaced onto the produced maps to indicate the boundaries of critical magmatic units in the study area. These correlations allow reasonable and meaningful interpretation for the reasons of high geothermal gradient and high heat-flow. In addition, a longitudinal seismic wave (V-p velocity) map was presented from the relationship between seismic velocity and radiogenic heat production in the western Anatolia, for the first time and they were correlated with the previous investigations. The estimated V-p velocities range from about 6 to 6.4 km/sn and low V-p values may be related to the partial melting of subducted structures in the western Anatolia. As a result, two new potential geothermal areas were determined by the integration of different methods used in this study. (C) 2015 Elsevier Ltd. All rights reserved.en_US
dc.language.isoengen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTDen_US
dc.relation.isversionof10.1016/j.geothermics.2015.12.002en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectCurie point depthen_US
dc.subjectHeat-flowen_US
dc.subjectMenderes Massifen_US
dc.subjectRadiogenic heat productionen_US
dc.subjectV-p velocitiesen_US
dc.titleCurie point depth, heat-flow and radiogenic heat production deduced from the spectral analysis of the aeromagnetic data for geothermal investigation on the Menderes Massif and the Aegean Region, western Turkeyen_US
dc.typearticleen_US
dc.relation.journalGEOTHERMICSen_US
dc.contributor.department[Bilim, Funda -- Akay, Tugce -- Kosaroglu, Sinan] Cumhuriyet Univ, Fac Engn, Geophys Engn Dept, TR-05480 Sivas, Turkey -- [Aydemir, Attila] Turkish Petr Corp, Sogutozu Mah,2180 Cad,10,Sogutozu, TR-06530 Ankara, Turkeyen_US
dc.identifier.volume60en_US
dc.identifier.endpage57en_US
dc.identifier.startpage44en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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