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dc.contributor.authorÖzer, Çağlar
dc.contributor.authorÖztürk, Serkan
dc.contributor.authorPamuk, Eren
dc.date.accessioned2023-01-25T07:21:56Z
dc.date.available2023-01-25T07:21:56Z
dc.date.issued2022en_US
dc.identifier.urihttps://journals.tubitak.gov.tr/cgi/viewcontent.cgi?article=1756&context=earth
dc.identifier.urihttps://hdl.handle.net/20.500.12440/5544
dc.description.abstractThe tectonic and structural properties of Erzurum and its surroundings have been investigated by evaluating the seismotectonic b -value, magnetic anomaly, edge detection analysis (total horizontal derivative (THDR) and tilt angle (TA)), Curie Point Depth (CPD), P-wave velocity (Vp), and Vp / Vs (S -wave velocity) ratio and by imaging the regional distributions of these parameters. For this purpose, all parameters have been combined to be able to reveal the new useful results on the study region and are presented for different locations and depths. The Vp values have been accompanied by high Vp / Vs ratios and shallow CPD values in the areas with geothermal regions such as Tekman, Soylemez, and the northern part of Karliova. In the tectonically active regions such as Ilica, Dumlu, Pasinler, cat, Karliova and Karacoban, high reduction -to - the -pole (RTP) total magnetic anomaly was accompanied by low Vp values in harmony. Besides, the low Vp values between 0 and 10 km and high b -values can be related to the weakness zones and the areas in which earthquake hazards are high in the study area. The low Vp values in the 0 km horizontal slice are in accordance with the high RTP total magnetic anomaly values in the triangle area between Askale, Ilica -Dumlu -Pasinler, Narman, and Karacoban. Uniformly, high Vp and low RTP total magnetic anomaly inclusions overlap in cat and Tekman. In some regions such as Dumlu, Narman, Horasan, Karacoban and south of Karliova, the tilt angle values are positive (positive values in the tilt angle map correspond to the center of the structure causing the magnetic anomaly) and the Vp values are low, but there is not a complete harmony between these parameters. These results show that variations on these parameters are related to each other, and these types of geophysical data are required for tectonic and structural features at different locations and depth levels.en_US
dc.language.isoengen_US
dc.publisherSCIENTIFIC TECHNICAL RESEARCH COUNCIL TURKEY-TUBITAKen_US
dc.relation.ispartofTURKISH JOURNAL OF EARTH SCIENCESen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectVp Vp Vs ratiob-value geothermal Curie point depthedge detectionen_US
dc.titleTectonic and structural characteristics of Erzurum and its surroundings (Eastern Turkey): a detailed comparison between different geophysical parametersen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Başka Kurum Yazarıen_US
dc.description.wospublicationidAAB-7300-2019en_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeofizik Mühendisliği Bölümüen_US
dc.identifier.volume31en_US
dc.identifier.issue1en_US
dc.identifier.startpage85en_US
dc.contributor.institutionauthorÖztürk, Serkan
dc.identifier.endpage108en_US
dc.description.wosqualityQ4en_US


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