• Journal of Korean Academy of Oral and Maxillofacial Radiology
• /
• v.19 no.1
• /
• pp.25-29
• /
• 1989

The author has evaluated the panoramic image clarity of the midfacial anatomic structures in dry skull according to the skull position. The radiopaque markers were attached to the anatomic structures: infraorbial rim, upper and lower borders of zygomatic arch, pterygomaxillary fissure, lateral pterygoid plate, pyriform aperture of nasal cavity, lateral wall of maxilla, orbital floor, infraorbital foramen, and nasal floor. Position of the skull were divided into four groups. standard, 25mm forward, chin-down, chin-up position. The results were as follows: 1. The pyriform aperture of nasal cavity, lateral wall of the maxilla, orbital floor, infraorbital foramen and nasal floor did net cast any discernible image. 2. Nearly all images of midfacial structures were blurred in the chin-up position. 3. The forward position provided good visualization of the maxillary sinus. 4. The chin-down position provided good visualization of the zygomatic arch, pterygomaxillary fissue, and lateral pterygoid plate.

• Journal of the Korean Association of Oral and Maxillofacial Surgeons
• /
• v.41 no.5
• /
• pp.281-283
• /
• 2015

Extraction of an impacted third molar is one of the most frequently performed techniques in oral and maxillofacial surgery. Surgeons can suffer numerous external injuries while extracting a tooth, with percutaneous injuries to the hand being the most commonly reported. In this article, we present a case involving a percutaneous injury of the surgeon's femoral region caused by breakage of the fissure bur connected to the handpiece during extraction of the third molar. We also propose precautions to prevent such injuries and steps to be undertaken when they occur.

• Archives of Craniofacial Surgery
• /
• v.19 no.1
• /
• pp.51-54
• /
• 2018

Post-traumatic scar deformations are common in many skin injury cases. These are usually aesthetic problems, but if these deformations impair mobility and the patient feels uncomfortable, we must resolve them. In a patient with a lateral post-traumatic scar fold in the lateral canthus that shortened the horizontal orbital fissure and created traction on eye opening, we performed modified classic Z-plasty, resulting in aesthetic and functional improvements without recurrence.

• The korean journal of orthodontics
• /
• v.16 no.2
• /
• pp.13-18
• /
• 1986

비강(nasal cavity)파 인두(pharynx)의 주기능의 하나는 상기도(upper respiratory tract) 로서 전비공(anterior nares)을 통해서 들이 마신 공기를 하기도(lower respiratory tract)로 통과시키는 기능이다. 일반적으로 홉기가 전비공에서 후비공(choana)으로 직선으로 통과하지 않고, 전비공에서 흡입된 공기는 후상방으로 높이 올라가 곡선으로 후열(olfactory fissure)을 향하여 후비공쪽으로 지나간다. 그러나 해부학적인 이상 즉, 비후된 비갑개 (turbinate), 아데노이드증식증(adenoid hyperplasia), 비중격만곡(deviation of the nasal septum)등의 여러가지 이 부위의 원인에 의하여 정상 비호흡이 어려워지면 만성 비폐색 (chronic nasal obstruction)이 생기게 되고 따라서 환자는 입이 반쯤 벌리고 구호흡(mouth breathing)을 하게 되며 우둔한 인상을 주고, 상악치아의 발육이상을 초래할 수 있다. 여기에 필자는 이비인후과 영역에서 구호홉을 초래할 수 있는 질환들에 관하여 약술하고자 한다.

• Archives of Plastic Surgery
• /
• v.43 no.4
• /
• pp.316-320
• /
• 2016

Cosmetic lateral canthoplasty, in which the size of the eye is increased by extending the palpebral fissure and decreasing the degree of the eye slant, has become a prevalent procedure for East Asians. However, it is not uncommon for there to be complications or unfavorable results after the surgery. With this in mind, the authors have designed a surgical method to reduce complications in cosmetic lateral canthoplasty by preserving the lateral canthal angle. We discuss here the anatomy required for surgery, the surgical methods, and methods for reducing complications during cosmetic lateral canthoplasty.

• Economic and Environmental Geology
• /
• v.18 no.1
• /
• pp.11-22
• /
• 1985

The Daehwa and Donsan tungsten-molybdenum deposits are composed of numerous fissure-filling veins developed in Precambrian gneiss and Cretaceous granite and quartz porphyry. K-Ar age of biotite in granite and that of muscovite in ore veins are $105{\pm}5\;Ma$ and 88.2~88.6 Ma respectively. Occurrence of ore deposits shows that relevant igneous rock is possibly quartz porphyry rather than above mentioned granite in temporal view point. Vein structure and mineralogy suggest that ore veins were formed by continuous vein filling, not by repeated mineralization. Three distinct depositional stages with decreasing age can be devided on the basis of mineral paragenesis and fluid inclusion studies: Stage I, deposition of oxides and silicates; stage II, deposition of base-metal sulfides and sulfosalts with carbonates; stage III, deposition of barren calcite and fluorite. Tungsten, molybdenum and tin mineralization occurred in stage I.

• Economic and Environmental Geology
• /
• v.16 no.3
• /
• pp.135-147
• /
• 1983

The copper deposits in Goseong district, Gyeongnam area are fissure filled copper veins emplaced on Cretaceous Goseong formation and andesitic rocks. Occurrence of ore veins and mineral paragenesis suggest a division of the hydrothermal mineralization into three stages: stage 1, deposition of arsenopyrite, pyrite, quartz, chlorite and epidote; stageII, deposition of pyrite, chalcopyrite, galena, sphalerite, electrum, pyrargyrite, tetrahedrite, silver sulfosalt minerals, quartz, chlorite, sericite and miner amount of calcite; stage III, formation of barren calcite veins. Filling temperature of fluid inclusions in quartz of stage II, range from 260 to 360 C and salinities from 6.2 to 13.6 weight percent NaCi equivalent.

• Economic and Environmental Geology
• /
• v.25 no.1
• /
• pp.17-25
• /
• 1992

South ore deposits of the Dunjeon gold mine is a fissure-filling vein emplaced in the Cretaceous granodiorite, skarnized and/or hornfelsified Ordovician Dumudong Formation. Mineralization can be divided into three distinct depositional stages on the basis of vein structure and mineral assemblages. Sb, Bi sulfosalts minerals, such as tetrahedrite, bournonite, boulangerite, cosalite, lillianite, heyrovskyite, unknown Pb-Bi-Sb-S mineral, native Sb, native Bi and Au-Ag minerals are mainly deposited in stage II. The formation temperature and sulfur fugacties of Sb, Bi minerals in the stage II deduced from thermodynamic considerations are from $172^{\circ}$ to $378^{\circ}C$ and $10^{-10.6}$ to $10^{-19.4}$ atm. Those temperatures are good agreement with temperature data obtained by fluid inclusion study which has reported already.

• Journal of The Korean Society of Inherited Metabolic disease
• /
• v.2 no.1
• /
• pp.1-6
• /
• 2002

출생 이후 머리둘레가 커지는 1개월 남아에게서 뇌초음파상 지주막하 공간이 확장되어 있고 백질의 음영이 증가되어 있었고 뇌 MRI 소견은 sylvian fissure의 확장과 양측 대뇌, 소뇌 피질과 백질이 T1 강조 영상에서 저신호강도와 T2 강조영상에서 고신호강도를 보였고 검사상 GA1 의심되었고 경피생검으로 얻은 섬유아세포 배양에서 glutaryl CoA dehydrogenase의 활성도가 전혀 없어 GA1을 확진하게 되었다. 이후 특수분유인 Glutatex(Abbott사) 수유와 riboflavin, carnitine 보충요법을 시행하여 대사성 위기나 급성 뇌증 위기는 없었고 양호히 발달하는 것을 경험하였기에 보고하는 바이다.

• The Journal of Engineering Geology
• /
• v.4 no.2
• /
• pp.127-138
• /
• 1994

The stationary dual-porosity model is not sufficient to describe the hydraulic characteristics of fractured aquifers as the groundwater flow in fractured aquifers is often controlled by the fractal geometry of fractures. This study deals with new stationary dual-porosity fractal model. This model simulates pseudo-steady state flow from matrix block to fissure in the fractal aquifer. Furthermore, it considers storage capacity and well loss effect at the production well. Type curves for different flow dimensions with different drainage factors are plotted. This new model has been applied to experimental data. The result of the interpretation shows a good accordance between the theoretical model and the observed data.