Sialoliths are calcified organic materials that forms in the salivary glands. Sialoliths are most commonly found in the submandibular gland, followed by the parotid gland. They are less common in the sublingual glands and minor salivary glands. Large sialoliths have been reported in the parenchyma of salivary glands and are often seen in 3-7 mm size. In this case report, 20x18 mm sialolith which is formed in hilum of submandibular salivary gland is presented together with the literature review
Sialolitler tükürük bezlerinde bulunan kalsifiye organik yapılardır. Tükürük bezi taşları en sık submandibular bezde görülmekle birlikte, ikinci sıklıkla parotis bezinde görülürler. Sublingual bezlerde ve minor tükürük bezlerinde daha nadir izlenirler. Literatürdeki olguların çoğu, bez parankiminde oluşan tükürük bezi taşlarından oluşmaktadır ve sıklıkla 3-7 mm boyutunda izlenirler. Bu makalede submandibular bez hilumunda oluşan, 20x18 mm boyutundaki submandibular tükürük bezi taşı literatür derlemesi ile birlikte sunulmaktadır
Primary Language | Turkish |
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Journal Section | Collection |
Authors | |
Publication Date | January 1, 2018 |
Published in Issue | Year 2018 Issue: 1 |
It is aimed that the Journal of International Dentistry Sciences be included in the Ulakbim TR Dizin. Necessary preparations are continuing for the issues to be published in 2020 in the TR Dizin.