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Electrical resistivity structure beneath MT. Erciyes Central Anatolia, Turkey

Yazıcı Bozkurt, Ruken. (Thesis (M.S.) - Bogazici University. Kandilli Observatory and Earthquake Research Institute, 2022., 2022)

The Central Anatolia (CA) is an intermediate belt between the Pontides and the Anatolide-Tauride blocks. Numerous basins, folds, faults, volcanic fields and rich mineral resources in the region have attracted the attention ...
Imaging fluid - rich zones by magnetotelluric method at south Marmara region

Cengiz, Özlem. (Thesis (M.S.) - Bogazici University. Kandilli Observatory and Earthquake Research Institute, 2012., 2012.)

Magnetotelluric data at sixteen sounding locations along two parallel profiles at south Marmara region were collected to improve the understanding of the crustal electrical conductivity structure. The PW (~40 km) and PE ...
Investigation of electrical conductivity characteristics at the vicinty of Genos fault, northwest Turkey by magnetotellurics

Karaş, Mustafa. (Thesis (M.S.)-Bogazici University. Kandilli Observatory and Earthquake Research Institute, 2017., 2017.)

As constituting the westernmost end of North Anatolian Fault, 45-km-long Ganos Fault acts as an active segment which represents a seismic gap. In this thesis, the ﬁrst systematic magnetotellurics observations are made to ...
The magnetotlluric phase tensor method for imaging the north Anatolian fault zone

Bekin, Ekrem. (Thesis (M.S.) - Bogazici University. Kandilli Observatory and Earthquake Research Institute, 2016., 2016.)

Magnetotelluric data often suffer from localized (three-dimensional) heterogeneities by a real and frequency independent phenomenon known as “galvanic distortions”. There have been numerous techniques developed for avoiding ...
The role of crustal fluids in tectonics of north-central Turkey inferred from three-dimensional magnetotellurics

Özaydın, Sinan. (Thesis (M.S.) - Bogazici University. Kandilli Observatory and Earthquake Research Institute, 2011., 2017.)

Central Pontides have been an active margin to Laurasia since the Paleozoic times. They consists of geological footprints of several episodes of subduction-accretion events and collisional tectonics. For these reasons, ...

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