YYÜ GCRIS Basic veritabanının içerik oluşturulması ve kurulumu Research Ecosystems (https://www.researchecosystems.com) tarafından devam etmektedir. Bu süreçte gördüğünüz verilerde eksikler olabilir.
 

Rhinolithiasis: Clinical, Radiological, and Mineralogical Features

dc.authorscopusid 23502609700
dc.authorscopusid 11239650700
dc.authorscopusid 24341667300
dc.authorscopusid 56260632500
dc.authorwosid Arslanoglu, Atilla/Aag-3542-2019
dc.contributor.author Yidirim, Nadir
dc.contributor.author Arslanoglu, Atilla
dc.contributor.author Sahan, Murat
dc.contributor.author Yidirim, Altan
dc.date.accessioned 2025-05-10T17:26:58Z
dc.date.available 2025-05-10T17:26:58Z
dc.date.issued 2008
dc.department T.C. Van Yüzüncü Yıl Üniversitesi en_US
dc.department-temp [Yidirim, Nadir] Yuzuncu Yil Univ, Fac Med, Dept Otolaryngol, TR-65100 Van, Turkey; [Arslanoglu, Atilla] Van Mil Hosp, Dept Radiol, Van, Turkey; [Sahan, Murat] Mevki Mil Hosp, Dept Otolaryngol, Ankara, Turkey; [Yidirim, Altan] Cumhuriyet Univ, Fac Med, Dept Otolaryngol, Sivas, Turkey en_US
dc.description.abstract Background: Rhinolithiasis is a rare and under-diagnosed clinical entity whose etiology and pathogenesis is poorly understood. Objective: The objective of the study is to review the clinical and radiologic features of rhinolithiasis and mineralogical-chemical composition of the rhinoliths with the aim of shedding light on its etiology and pathogenesis. Methods: Our subjects consisted of 8 rhinolithiasis cases. Clinical presentations, signs, and symptoms of the patients with radiologic findings are presented, and X-ray diffraction analyses of the stones were carried out to assess their mineralogical composition. Results: Nasal obstruction appeared to be the chief symptom, followed by nasal discharge and facial pain. Neither exogenous nor endogenous nidi were identified in any of the cases. Mineralogical analyses of the rhinoliths revealed Whitlockite [(Ca,Mg)3 (PO4)2] in one and Dahllite [Ca5 (PO4,CO3)3OH] in 7 cases. Conclusion: We hypothesized that some substances or organic objects form the nidi of the rhinoliths and are disintegrated over the course of mineral precipitation. This hypothesis was supported by radiologic and microscopic findings. en_US
dc.description.woscitationindex Science Citation Index Expanded
dc.identifier.doi 10.2500/ajr.2007.21.3112
dc.identifier.endpage 81 en_US
dc.identifier.issn 1050-6586
dc.identifier.issue 1 en_US
dc.identifier.pmid 17976254
dc.identifier.scopus 2-s2.0-39749130958
dc.identifier.scopusquality N/A
dc.identifier.startpage 78 en_US
dc.identifier.uri https://doi.org/10.2500/ajr.2007.21.3112
dc.identifier.uri https://hdl.handle.net/20.500.14720/11834
dc.identifier.volume 22 en_US
dc.identifier.wos WOS:000253232100015
dc.identifier.wosquality N/A
dc.language.iso en en_US
dc.publisher Ocean Side Publications inc en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.subject Calcification en_US
dc.subject Calculi en_US
dc.subject Computerized Tomography en_US
dc.subject Foreign Body en_US
dc.subject Imaging en_US
dc.subject Nasal Cavity en_US
dc.subject Nidus en_US
dc.subject Rinolithiasis en_US
dc.subject Rhinoliths en_US
dc.subject X-Ray Diffraction en_US
dc.title Rhinolithiasis: Clinical, Radiological, and Mineralogical Features en_US
dc.type Article en_US

Files