Atıf İçin Kopyala
Başokur A. T., Meqbel N., Hacıoğlu Ö., Arslan H. İ., Efeçınar T.
10th Congress of Balkan Geophysical Society, Albena, Bulgaristan, 18 - 22 Eylül 2019, ss.1-5
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Yayın Türü:
Bildiri / Özet Bildiri
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Doi Numarası:
10.3997/2214-4609.201902617
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Basıldığı Şehir:
Albena
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Basıldığı Ülke:
Bulgaristan
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Sayfa Sayıları:
ss.1-5
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Karadeniz Teknik Üniversitesi Adresli:
Evet
Özet
A magnetotelluric survey has been conducted in Cappadocia
region of central Turkey in order to find new geothermal resources. The survey
area has formerly been postulated as the location of a buried caldera that was
one of the main eruptive centres of Cappadocia volcanic province.
Three-dimensional non-linear conjugate gradient inversion of magnetotelluric
data by using the full impedance tensor helps to delineate the subsurface resistivity
distribution. The derived resistivity model reveals the possibility of a buried
caldera. The low resistivity anomalies are interpreted as the clay alteration
zones caused by hydrothermal activities.A magnetotelluric survey has been conducted in Cappadocia
region of central Turkey in order to find new geothermal resources. The survey
area has formerly been postulated as the location of a buried caldera that was
one of the main eruptive centres of Cappadocia volcanic province.
Three-dimensional non-linear conjugate gradient inversion of magnetotelluric
data by using the full impedance tensor helps to delineate the subsurface resistivity
distribution. The derived resistivity model reveals the possibility of a buried
caldera. The low resistivity anomalies are interpreted as the clay alteration
zones caused by hydrothermal activities.