Coulomb Stress Analysis in Nemrut Caldera (East Anatolia, Türkiye)

dc.contributor.authorAlkan, Hamdi
dc.contributor.authorBektaş, Özcan
dc.contributor.authorBüyüksaraç, Aydın
dc.date.accessioned2024-10-26T17:37:43Z
dc.date.available2024-10-26T17:37:43Z
dc.date.issued2024
dc.departmentSivas Cumhuriyet Üniversitesi
dc.description.abstractIn volcanic areas, seismic events with low energy occur before seismic activity or due to the movement observed in the magma. These earthquakes, which are caused by the expansion-contraction movement that has been revealed in different studies and is mostly observed in the magma chamber, can be recorded with continuous observations. On the other hand, it is not easy to distinguish between tectonic and volcanic origins of earthquakes occurring in volcanic areas. In this study, Coulomb stress analysis was carried out using earthquakes in the Nemrut Stratovolcano, which is located in the eastern Türkiye and is at the westernmost end of a volcano arc, and it was concluded that the stress is related to the Nemrut Caldera, therefore the positive stress caused by the expansion of the magma chamber of the Nemrut Volcano creates tremors.
dc.identifier.doi10.17798/bitlisfen.1491872
dc.identifier.endpage797
dc.identifier.issn2147-3129
dc.identifier.issn2147-3188
dc.identifier.issue3
dc.identifier.startpage788
dc.identifier.trdizinid1267352
dc.identifier.urihttps://doi.org/10.17798/bitlisfen.1491872
dc.identifier.urihttps://search.trdizin.gov.tr/tr/yayin/detay/1267352
dc.identifier.urihttps://hdl.handle.net/20.500.12418/23579
dc.identifier.volume13
dc.indekslendigikaynakTR-Dizin
dc.language.isoen
dc.relation.ispartofBitlis Eren Üniversitesi Fen Bilimleri Dergisi
dc.relation.publicationcategoryMakale - Ulusal Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectNemrut Caldera
dc.subjectSeismicity
dc.subjectVolcano
dc.subjectCoulomb Stress
dc.titleCoulomb Stress Analysis in Nemrut Caldera (East Anatolia, Türkiye)
dc.typeArticle

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