Geothermal Prospectivity of the Bigadic Basin and Surrounding Area, Nw Anatolia, Turkey, by the Spectral Analysis of Magnetic Data

dc.authorscopusid12801104200
dc.authorscopusid15029792400
dc.authorscopusid36927494500
dc.contributor.authorBilim, Funda
dc.contributor.authorAydemir, Attila
dc.contributor.authorAtes, Abdullah
dc.date.accessioned2024-07-05T15:19:42Z
dc.date.available2024-07-05T15:19:42Z
dc.date.issued2021
dc.departmentAtılım Universityen_US
dc.department-temp[Bilim, Funda] Cumhuriyet Univ, Engn Fac, Geophys Engn Dept, TR-05480 Sivas, Turkey; [Aydemir, Attila] Turkish Petr Corp, 2180 Cad 10, TR-06530 Ankara, Turkey; [Aydemir, Attila] Atilim Univ, Engn Fac, Energy Syst Engn Dept, Ankara, Turkey; [Ates, Abdullah] Ankara Univ, Engn Fac, Geophys Engn Dept, TR-06100 Ankara, Turkeyen_US
dc.description.abstractThe Curie Point Depths (CPDs) are estimated from the spectral analysis of magnetic data in order to determine the geothermal potential of the Bigadic Basin and its surrounding region in NW Anatolia, Turkey. The estimated CPD range is from 7 to 17-18 km. The shallowest depth (7 km) lies to the north of Balikesir. The estimated geothermal gradient and heat flow values range from 33 to 80 degrees C/km, and 83 to 200 mWm(-2), respectively. All results in the study area support the previous studies from the geological or geophysical investigations for western Anatolia by other researchers. High temperatures may be resulted indirectly from the continental collision and consequent thermal relaxation and/or heating from the interiors of the Earth due to the mantle delamination or asthenospheric upwelling in response to lithospheric extension in the western Anatolia. The high heat flow and shallow CPDs can also be associated with the magmatic rocks as a consequence of the recent tectonic extension and granitoids in the studied region.en_US
dc.identifier.citation1
dc.identifier.doi10.1007/s00024-021-02787-y
dc.identifier.endpage3107en_US
dc.identifier.issn0033-4553
dc.identifier.issn1420-9136
dc.identifier.issue8en_US
dc.identifier.scopus2-s2.0-85108117825
dc.identifier.startpage3085en_US
dc.identifier.urihttps://doi.org/10.1007/s00024-021-02787-y
dc.identifier.urihttps://hdl.handle.net/20.500.14411/2007
dc.identifier.volume178en_US
dc.identifier.wosWOS:000662819000002
dc.identifier.wosqualityQ3
dc.language.isoenen_US
dc.publisherSpringer Basel Agen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectCurie point depthen_US
dc.subjectmagnetic anomalyen_US
dc.subjectBigadic Basinen_US
dc.subjectheat flowen_US
dc.subjectanalytic signalen_US
dc.subjectBalikesiren_US
dc.titleGeothermal Prospectivity of the Bigadic Basin and Surrounding Area, Nw Anatolia, Turkey, by the Spectral Analysis of Magnetic Dataen_US
dc.typeArticleen_US
dspace.entity.typePublication

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