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dc.contributor.authorKocasarac, Husniye Demirturk
dc.contributor.authorCelenk, Peruze
dc.contributor.authorErzurumlu, Zerrin
dc.contributor.authorKutlar, Gokhan
dc.date.accessioned2020-06-21T14:05:02Z
dc.date.available2020-06-21T14:05:02Z
dc.date.issued2013
dc.identifier.issn2212-4403
dc.identifier.urihttps://doi.org/10.1016/j.oooo.2013.05.019
dc.identifier.urihttps://hdl.handle.net/20.500.12712/15763
dc.descriptionERZURUMLU, ZERRIN UNAL/0000-0002-8693-1206en_US
dc.descriptionWOS: 000321737900026en_US
dc.descriptionPubMed: 23849377en_US
dc.description.abstractRhinoliths are calcified masses in the nasal cavity caused by the deposition of nasal, lacrimal, and inflammatory mineral salts by accretion around an endogenous or exogenous nidus. Rhinoliths can be seen as incidental findings on panoramic radiography, although they typically appear blurred due to remaining outside the focus. Therefore, rhinoliths may be difficult to recognize; this difficulty can lead to misdiagnosis. Computed tomography (CT)/cone beam CT (CBCT) scans are generally necessary to define the precise location and to make a differential diagnosis. This article describes radiologic features of five cases of rhinoliths that were detected incidentally on panoramic radiographs. CT or CBCT images were obtained before removing the rhinoliths.en_US
dc.language.isoengen_US
dc.publisherElsevier Science Incen_US
dc.relation.isversionof10.1016/j.oooo.2013.05.019en_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titleClinical and radiological aspects of rhinoliths: report of five casesen_US
dc.typearticleen_US
dc.contributor.departmentOMÜen_US
dc.identifier.volume116en_US
dc.identifier.issue2en_US
dc.identifier.startpage232en_US
dc.identifier.endpage237en_US
dc.relation.journalOral Surgery Oral Medicine Oral Pathology Oral Radiologyen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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