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Menetrier 병에 동반된 낭성 심재성 위염 1 예
이방희,박미자,최호순,고정희,최덕례,박강서,박기현,성시경,김덕기,류창수,이현상,강윤중 대한내과학회 1995 대한내과학회지 Vol.48 No.6
Menetrier's disease, hypertrophec gastritis or hypertophic gastropathy, with mucosal hypertrophy in which the enlarged gastric rugae involved part or all of the stomach giving the appearance of cerebral convolutions. The enlarged rugae which characterize this disease are not attributable to lymphoma, infiltrative carcinoma or non-neoplastic disease, such as syphilis, tuberculosis kor sarcoidosis. Most impressive of Histologic features if the expanded or thickened mucosa, are mostly to an elongation of the foveolae, which become tortuous or corkscrew. Often these elongated pits will extended to the base of the mueosa where they may become cystic. On occasion, the deep cysts may apper to penetrate the muscularis mucosae and extend into the superficial submucosa, where they are surrounded by bundles of smooth muscle, another example of gastric cystica profunda. Gastritis cystica profunda is a rare condition in which mature glandular epithelium extends into the tissues beneath the muscularis in which mature glandular epithelium extends into the tissues beneath the muscularis mucosae. Benign gastric pseudotumor, gastritis cystica profunda, posses malignant histological features but functionally benignly. It is an analogous to similiar conditions affecting the small and large intestines that are called, repectively, enteritis and colitis cystica profunda. The proposed pathogenesis of these abnormalities relates to ischemia, chronic inflammation, and the presence of a foreign body. We present a case of Menetrier's disease assocated with gastritis cystica profunda and a brief review of clinical and pathologic pictures and management.
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이방희(Lee Bang-Hee),김진호(Kim Jin-Ho) 한국마린엔지니어링학회 2007 한국마린엔지니어링학회 학술대회 논문집 Vol.2007 No.-
The Habeol sandy body is a tidal sand ridge located in the Gyeonggi Bay, which is macrotidal environment with tidal ranges of up to 9m(Park, 2006). This sandy body is characterized as a bugle-shape which is getting narrower toward NE with 9.2㎞ length and 5.4 ~ 0.8㎞. This is present in water -3 ~ 3lm(below DLI)) and has trough(> 35m DL) in the each side. As a result of sub-bottom profile analysis, this deposits are consist of three seismic unit(Unit Ⅰ, Ⅱ, Ⅲ). Interpretation of seismic and lithologic data has shown that the regional sea-level changes are not only play a major role in the evolution of sand body and the seabed topography and tidal flow have achieved regime existence of sand body in the presenu about(< 5,000yr B.P.).