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dc.contributor.authorSayin, Nurdan
dc.date.accessioned2021-03-03T18:41:56Z
dc.date.available2021-03-03T18:41:56Z
dc.identifier.citationSayin N., "THE HEAT PRODUCTION BY RADIOACTIVE ELEMENTS IN THE MARMARA REGION", 11th International Multidisciplinary Scientific GeoConference, Albena, Bulgaristan, 20 - 25 Haziran 2011, ss.181-187
dc.identifier.othervv_1032021
dc.identifier.otherav_508204c4-ab61-477f-a235-cc17df10d049
dc.identifier.urihttp://hdl.handle.net/20.500.12627/57311
dc.description.abstractThe main two sources that contribute to the surface heat flow density value are (1) heat production within the crust due to decay of unstable isotopes of Uranium 238 (U), Thorium 232 (Th), Potassium 40 (K), and (2) heat flow density from the mantle. Heat production can be calculated using the regional radioactive U, Th and K values. In this study radiogenic heat production values were estimated from U238, Th232 and K40 concentrations from Marmara Region. The crustal temperature distribution has been modelled by the measured values of temperature gradient wells in the region and temperature values in crust and mantle boundary were obtained. The mechanical behavior characteristics and composition of the crust were revealed by correlating earthquake depth in region and heat modeling data.
dc.language.isoeng
dc.subjectMühendislik ve Teknoloji
dc.subjectJEOLOJİ
dc.subjectJeoloji Mühendisliği
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectYER BİLİMİ, MULTİDİSİPLİNER
dc.titleTHE HEAT PRODUCTION BY RADIOACTIVE ELEMENTS IN THE MARMARA REGION
dc.typeBildiri
dc.contributor.departmentİstanbul Üniversitesi , Mühendislik Fakültesi , Jeofizik Müh. Böl.
dc.contributor.firstauthorID55556


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