• Economic and Environmental Geology
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• v.31 no.3
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• pp.171-183
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• 1998

Early Tertiary volcanics, volcanoclastics and granodiorite occur in the Barton Peninsula, King George Island, Antarctica. In the granodioritic stock and volcanic rocks, propylitic alteration characterized by actinolite, epidote, chlorite and calcite is widespread, and disseminations and veinlets of sulfide minerals such as pyrite, chalcopyrite and bornite are ubiquitious. The study on the hydrothermal alteration near granodioritic stock can be summarized as follows; (1) granodiorite intrusion is a small, high level stock associated with calc-alkaline volcanism, and have high copper content, (2) high temperature type of propylitic alteration and common occurrence of copper sulfides in and around granodiorite intrusion, (3) low ${\delta}^{34}S$ values of pyrites by oxidational conditions of sulfide deposition, (4) low ${\delta}^{34}S$ values of quartz and feldspar in the granodiorite, and isotopic non-equilibrium by hydrothermal alteration. It suggest that hyrothermal alteration and mineralization near granodioritc stock should be genetically related to granodiorite intrusion in the Barton Peninsula.

• The Korean Journal of Zoology
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• v.28 no.4
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• pp.211-226
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• 1985

The ultrastructure of the digestive organ of Korean Planaria (Dugesia japonica) is studied by light microscope and transmission electron microscope. 1. Pharynx The epithelium surrounding pharyngeal lumen has a number of microvilli on the free surface. The epithelial cells contain PAS-positive granules which are 0.4 to 0.6 $\\mum$ in size. They also contain hundreds of vesicles and vacuoles. The pharyngeal epithelium of the external surface surrounded by pharyngeal cavity possesses a number of cilia and microvilli on the free surface. A number of muscle bundles are found in the pharyngeal tissue. The parietal epithelium surrounding pharyngeal cavity have microvilli and electron-dense secretory granules. 2. Caeca The cells which constitute the cecal epithelium are divided into four kinds of cells. 1) Phagocytic cell : These cells are characterized by presence of a number of lysosomes. These cells have highly developed mitochondria, polyribosomes and granular endoplasmic reticulum of which cisternae are distended. 2) Granular club cell : These cells contain round granules 5 $\\mum$ in diameter which show strong PAS-positivity and weak eosinophilia. The cells have highly developed granular endoplasmic reticulum. 3) Storage cell : These cells include thousands of glycogen granules in the cytoplasm. These cells also have second kind of round granules which are 1.4 to 3 $\\mum$ in size and exhibit PAS-positive reaction. 4) Immature storage cell : These cells have a large nucleus and contain a small number of granules which have PAS-positive granules and a few lipid droplets. Several chromatoid bodies are found in the cytoplasm around the nucleus.

• The Journal of the Petrological Society of Korea
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• v.16 no.3
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• pp.162-179
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• 2007

Macheon Layered Intrusion (MLI) which intruded into Precambrian gneiss complex of the northern Jirisan area, southeastern part of Youngnam (or Sobaeksan) Massif, is a layered mafic-ultramafic complex of Triassic age (ca. 223 Ma). The MLI is divided into Layered Series and Laminated Series. Layered Series is subdivided into Central Zone (Lower Zone) consisting of olivine gabbros and Peripheral Zone (Middle or Upper Zone) consisting of hornblende gabbros based on the type of cumulus texture and the main mafic phase. The Central Zone of Layered Series comprises thinly laminated olivine gabbros and uniform or thickly laminated coarse olivine gabbros which consist of mela-gabbro, troctolite, leuco-troctolite, and anorthositic rocks. Laminated Series is also subdivided into quartz-bearing biotite-pyroxene gabbros and homblende diorite and both have variable amount of interstitial quartz and microcline. Laminated series display moderately to slightly developed igneous lamination which is defined by the planar alignment of lath-shape plagioclases. Chilled margin of quartz-bearing biotite-pyroxene gabbro with surrounding Precambrian gneisses insists shallower intrusion of more felsic cognate magma evolved in the deep a little later. Rocks of Layered Series have orthocumulus to adcumulus olivine, adcumulus to intercumulus plagioclase, and intercumulus to heteradcumulus pyroxene and hornblende. Magmatic modally grading, folding, and cross-lamination are not rarely occurred in thinly layered rocks. These textural characteristics define main mechanisms of the formation of layered and laminated structure in mafic-ultramafic rocks of Macheon Layered Intrusion are gravity settling and in-situ crystallization associated with slumping and density current.

• The Journal of Korean Academy of Prosthodontics
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• v.55 no.4
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• pp.410-418
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• 2017

Amelogenesis imperfecta characterized as abnormally formed enamel is caused by a defect of unique group of genes. Patients affected by this disease might have difficulties in social and psychological aspects due to non-esthetic teeth as well as functional problems caused by enamel detachment and tooth wear from their early ages. Adult patients with amelogenesis imperfecta can be treated with full-mouth restorations, which make functional and esthetic rehabilitations of severely worn tooth. However, the anterior open bite and lack of occlusal clearance for posterior teeth restorations due to compensatory extrusion are the intervening factors in the prosthetic treatment. Therefore, the determination of anterior tooth lengths, vertical dimension, and anterior guidance should be set carefully. Recently, computer-aided design and computer-aided manufacturing (CAD/CAM) techniques help systematic approaches and enable dentists to reduce time-consuming procedures in the diagnosis and treatment of full-mouth rehabilitation. This case report demonstrates the successful full mouth rehabilitation using a CAD/CAM system in a young adult patient with amelogenesis imperfecta and anterior open bite.

• KAPE Magazine
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• s.155
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• pp.8-8
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• 2009

• KAPE Magazine
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• s.199
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• pp.16-16
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• 2013

• KAPE Magazine
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• s.197
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• pp.14-14
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• 2013

• Proceedings of the Korean Society of Crop Science Conference
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• 1983.05a
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• pp.32-32
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• 1983

• KAPE Magazine
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• s.261
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• pp.20-21
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• 2018

• Proceedings of the Korean Society of Sericultural Science Conference
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• 2000.10a
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• pp.71-71
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• 2000