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

dc.authorscopusid 12801104200
dc.authorscopusid 15029792400
dc.authorscopusid 36927494500
dc.contributor.author Bilim, Funda
dc.contributor.author Aydemir, Attila
dc.contributor.author Ates, Abdullah
dc.date.accessioned 2024-07-05T15:19:42Z
dc.date.available 2024-07-05T15:19:42Z
dc.date.issued 2021
dc.department Atılım University en_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, Turkey en_US
dc.description.abstract The 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.citationcount 1
dc.identifier.doi 10.1007/s00024-021-02787-y
dc.identifier.endpage 3107 en_US
dc.identifier.issn 0033-4553
dc.identifier.issn 1420-9136
dc.identifier.issue 8 en_US
dc.identifier.scopus 2-s2.0-85108117825
dc.identifier.startpage 3085 en_US
dc.identifier.uri https://doi.org/10.1007/s00024-021-02787-y
dc.identifier.uri https://hdl.handle.net/20.500.14411/2007
dc.identifier.volume 178 en_US
dc.identifier.wos WOS:000662819000002
dc.identifier.wosquality Q3
dc.language.iso en en_US
dc.publisher Springer Basel Ag en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.scopus.citedbyCount 4
dc.subject Curie point depth en_US
dc.subject magnetic anomaly en_US
dc.subject Bigadic Basin en_US
dc.subject heat flow en_US
dc.subject analytic signal en_US
dc.subject Balikesir en_US
dc.title Geothermal Prospectivity of the Bigadic Basin and Surrounding Area, Nw Anatolia, Turkey, by the Spectral Analysis of Magnetic Data en_US
dc.type Article en_US
dc.wos.citedbyCount 5
dspace.entity.type Publication

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