• Proceedings of the Korea Contents Association Conference
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• 2011.05a
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• pp.99-100
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• 2011

21세기에 들어서면서 급속도로 성장한 한국의 게임 산업은 어느덧 국내에서 성숙기 단계를 맞이하고 있다. 또한 게임 산업의 꾸준한 확장을 위해서는 글로벌 시장에서 인정받을 수 있는 게임 개발이 절실히 요구되고 있다. 본 논문은 이를 위한 한 단계로서 MMORPG 장르의 게임 중에 오랫동안 이 분야에서 성공 가도를 달리고 있는 월드오브워크래프트를 몰입도 관점에서 성공 요인을 분석하고, 이를 바탕으로 2011년도에 주목 받고 있는 신생 게임 테라의 특징을 동일한 관점에서 분석한다. 몰입도 분석 방법은 정보이론과 정신물리학에 기반하며 게임의 레벨과 스킬의 개수에 의존적인 함수로서 정량적인 접근 방법을 제안한다. 제안 방법에 따르면 월드오브워크래프트는 확장팩 대격변을 전후하여 레벨에 따른 스킬 콘텐츠를 재배치하여 새로운 시도를 선보였다. 그 반면에 테라는 화려한 그래픽을 강점으로 내세우지만 낮은 몰입도와 레벨에 따른 스킬 콘텐츠가 부족하고 그 의도마저 모호하다. 이러한 특징은 실제 테라를 플레이할 때 나타나는데 월드오브워크래프트에 비해 상대적으로 단조로운 스킬 선택권과 직업 선택권의 형태로 발견되어지는 문제로서 제안하는 방법이 몰입도를 측정하는 하나의 방법으로 평가된다.

• Journal of the Speleological Society of Korea
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• v.24 no.25
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• pp.30-68
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• 1991

제주도는 지리적으로 동경 126$^{\circ}$08'～126$^{\circ}$58', 북위 33$^{\circ}$06'～34$^{\circ}$00'에 위치하며 비양도, 우도, 상추자도, 하추자도, 횡간도, 가파도, 마라도 등 8개의 유인도와 54개의 무인도로 구성되었으며 행정구역상 2시 2군 6읍 5면으로 되어 있다. 또한 본 도는 한반도의 최남단에 위치하며 환태평양 조산대 즉 호상열도에서 벗어난, 대륙쪽에 위치한 화산도로서 백두산, 울릉도, 연천, 전곡 지역 등과 더불어 신생대화성활동과 그에 수반하여 생성된 화산용암 동굴에 관한 연구조사 지역으로 대단히 의의가 있는 대상이다.(중략)

• The Journal of Engineering Geology
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• v.26 no.1
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• pp.33-49
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• 2016

The study area, located in Sinam-ri, Ulsan, in the southeastern part of the Korean Peninsula, is mainly composed of hornblende granite (ca. 65 Ma). Fracturing and reactivation of a fault striking ENE-WSW was strongly controlled by the intrusion of a mafic dyke (ca. 44 Ma), which behaves as a discontinuity in the mechanically homogeneous pluton, increasing the instability of the basement in this area. A geometric and kinematic study undertaken to interpret the faults and fractures was performed in a trench excavated almost perpendicular to the orientation of the dyke. The analysis of structural elements, such as dykes, veins, and faults, is used to infer the deformation history and to determine the paleostress orientations at the time of formation of the structures. The deformation history established based on this analysis is as follows: (1) NNE-SSW, E-W, ENE-WSW, and NE-SW trending fractures had already developed in the pluton before dyke intrusion; (2) felsic dykes intruded under conditions of σ_Hmax oriented N-S and σ_Hmin oriented E-W; (3) mafic dykes intruded under conditions of σ_Hmax oriented E-W and σ_Hmin oriented N-S; (4) dextral reactivation of the main fault associated with the development of hydrothermal quartz veins under conditions of σ_Hmax oriented E-W and σ_Hmin oriented N-S; (5) sinistral reactivation of the main fault and high-angle normal faults under conditions of σ_Hmax oriented NE-SW and σ_Hmin oriented NW-SE; and (6) dextral reactivation of the main fault and NE-SW low-angle reverse faults under conditions of σ_Hmax oriented NW-SE and σ_Hmin oriented NE-SW. These results are consistent with the tectonic history of the Pohang-Ulsan block in the southeastern part of the Korean Peninsula, and indicates the tectonic deformation of the southern area of the Ulsan fault bounded by Yangsan fault was analogous to that of the Pohang-Ulsan area from the Cenozoic. This work greatly aids the selection of sites for critical facilities to prevent potential earthquake hazards in this area.

• Journal of the Korean earth science society
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• v.21 no.3
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• pp.230-249
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• 2000

Southeastern Korean Peninsula has undergone the polyphase deformations according to the changes of regional tectonic settings during the Cenozoic. Through analyses of more than 600 fault-slip data gathered in the study area, five tectonic events are revealed as the followings: (I) NW-SE transtension, (II) NW-SE transpression, (III) NE-SW pure or radial extension, (IV) NNE-SSW transpression, (V) NE or ENE-WSW transpression. Event I was induced by the pull-apart type extension of the East Sea during 24-16 Ma, which resulted in the NW-SE extension of the Tertiary Basins in SE Korea. Event II was resulted from the collision of SW Japan and Izu-Bonnin Arc (or Kuroshio Paleoland) on the Philippine Sea Plate at ${\sim}$ 15 Ma, which stopped the extension of the Tertiary Basins and originated the uplift of fault blocks in and around SE Korean Peninsula. It was continued until ${\sim}$ 10 Ma. Event III is interpreted as the post-tectonic event after the block-uplifts due to the event II, which indicates a temporal lull in activity of the Philippine Sea Plate since 10 Ma. Event IV was originated from the resumption in activity of the Philippine Sea Plate which was restarted to move toward north at ${\sim}$ 6 Ma. The event made the EW compressional structures behind SW Japan as well as in the Korea Straits, and thus the block-uplifts in SE Korea was resumed again. Lastly, event V was resulted from the gradual decrease in influence of the Philippine Sea Plate and the cooperative compression due to the subduction of the Pacific Sea Plate and the collision of the Indian Plate since 5-3.5 Ma, which generated the NS compressional structures in the offshore along the eastern coast of the Korean Peninsula and thrust up the fault-blocks toward west. This event is continuing so far, and thus is making the active faultings resulting in the present earthquakes of the Korean Peninsula.

• The Journal of Engineering Geology
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• v.32 no.1
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• pp.113-126
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• 2022

The tectonic history of the Chukchi Abyssal Plain in the Amerasia Basin, Arctic Ocean, has not been fully explored due to the harsh conditions of sea ice preventing detailed observation. Existing models of the tectonic history of the region provide contrasting interpretation of the timing of formation of the crust (Mesozoic to Cenozoic), crust type (from hyper-extended continental crust to oceanic crust), and formation process (from parallel/fan-shaped rifting to transformation faulting). To help determine the age of the oceanic crust, the geothermal gradient was measured at three stations in the south of abyssal plain at depth of 2,160-2,250 m below sea level. Heat flow measurement stations were located perpendicular to the spreading axis over a 40 km-long transect. In-situ thermal conductivity measurement, corrected by the laboratory test, gave observed marine heat flows of 55 to 61 mW/m². All measurements were taken during Arctic expeditions in 2018 (ARA09C expedition) and 2021 (ARA12C expedition) by the Korean ice-breaking research vessel (IBRV) Araon. Given the assumption of oceanic crust, the results correspond to formation in the Late Cretaceous (Mesozoic). The inferred age supports the hypothesis of formation activated by the opening of the Makarov Basin during the Late Mesozoic-Cenozoic. This would make it contemporaneous with rifting of the Chukchi Border Land immediately east of the abyssal plain. The heat flow data indicate the base of the gas hydrate stability zone is located 332-367 m below the seafloor, this will help to identify the gas hydrate-related bottom simulating reflector in the future seismic survey, as already identified on the Chukchi Plateau. Further geophysical surveys, including heat flow measurements, are required to increase our understanding of the formation process and thermal mantle structure of the abyssal plain.

• Journal of agricultural medicine and community health
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• v.30 no.1
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• pp.1-14
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• 2005

Objectives: This study attempts to analyze the length of hospital stay and expenses of frequent disease admitted in a Vaterans Hospital. Methods: Data was collected from January 1, 2001 to December 31, 2003 from the Claim records of 9,640 patients in a Vaterans Hospital. Results: The results were as follows: 1. In age & sex distribution, there was male 70.9%, female 29.1%, and 35.8% of them is 70 age group. Frequency by insurance program was Health insurance 78.1%, Medical aid 14.2%, no insurance 4.1%, others 3.6%. Distribution of each department was internal medicine 28.3%, orthopedic surgery 21.3%, surgery 16.6%, neurosurgey 7.1%, pediatrics 5.9%. Also, in the veterans group, male to female patient ratio was 99.3% male to 0.7% female, them over 70 years old was 51.6%, and them which live in daejeon was 43.5%. 2. In frequency of disease, there was gastroenteritis 4.8%, pneumonia 3.8%, cartaract 3.7%, cerebral infarct 3.2%, hyperplasia of prostate 3.0%. In frequency of korean standard classification of diseases, there was injury and poisoning and certain other consequences of external causes 17.1%, diseases of digestive system 16.1%, diseases of musculoskeletal system and connective tissue 13.9%, diseases of respiratory system 9.4%, diseases of genitourinary system 8.6%. Also, in veterans group, frequency of them was diseases of musculoskeletal system and connective tissue 19.4%, diseases of digestive system 16.8%, injury and poisoning and certain other consequences of external causes 15.7%, diseases of genitourinary system 9.7%, diseases of circuatory system 8.2%. 3. Average length of hospital stay was 29.0 days for total patients, 51.8 days for the veterans group, 15.7 days for the non-veterans one. Average total expenses was 3,669,579 won, the veterans group 7,263,877 won, the non-veterans one 1,560,333 won. The ratio of insurer to insuree was 55.2 : 44.8, the ratio of amount paid by patient in the veterans group 61.7%, in the non-veterans one 33.0%. 4. In items of medical expenses, fee for hospital accommodation was 34.7%, fee for medication 13.2%(injection 7.8%, drug 5.4%), fee for service 48.6%(physical therapy 26.3%, operation 9.7%, laboratory examination 5.2%, radiological examination 3.1%, etc), others 3.4%. In them for the veterans group, fee for physical therapy was 35.3%, fee for hospital accommodation 35.2%, fee for injection 6.2%, fee for operation 5.9%, for the non-veterans one, fee for hospital accommodation 35.7%, fee for operation 16.4%, fee for injection 11.4%, fee for laboratory examination 8.3%. 5. In the comparison of the frequency by Korean standard classification of diseases and distance between the hospital and home, the region under 21.5Km was more frequent in symptoms, signs an abnormal clinical and laboratory findings 56.0%, injury and poisoning and certain other consequences of external causes 55.6%, diseases of the eye and adnexa 52.9%, the one over 21.5Km was more frequent in neoplasms 57.4%, diseases of musculoskeletal system and connective tissue 55.9%, diseases of genitourinary system 53.5%.

• Journal of the Korean Geographical Society
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• v.43 no.6
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• pp.775-790
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• 2008

This study shows possibility of active fault, throughout analyzing distributional features of tectonic and fluvial geomorphology and mineral composition of fault fracture clay, at Jinbu fault-line system in Pyeongchang-gun, Gangwon Province. Fault-line valley was formed remarkably in the upper reaches of Odae River and upper reaches of Yeongok River according along Jinbu fault-line. Landforms show rectilineal distribution at right shore slopes of Odae River in Ganpyeong-ri, southern zone of Jinbu fault-line system, related to the tectonic processes, such as triangular facet, kernbut, kerncol and alluvial fan. Fault fracture clay zones were developed at 5 outcrops($jbf1{\sim}5$), located in kerncol. Particularly, jbf1 fault outcrop, developed at granite saprolite, has obvious fault plane and fault clay composed of illite and laumontite. The Jinbu Fault-line along jbf4-2-3-5 may be formed by regional compressive stress, and jbf1 fault may be suggested a tributary fault of the Jinbu fault-line formed before the late Pleistocene. The vertical displacement of the east and west blocks of the Jinbu Fault-line is estimated in $0.024{\sim}0.027m/ka$.

• Ocean and Polar Research
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• v.26 no.2
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• pp.245-253
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• 2004

The Intertropical Convergence Zone (ITCZ), where the southeast and northeast trade winds converge, is the effective climatological barrier that separates the southern and northern hemispheres in dust budget. Asian and N. American dusts dominate in fhe Pacific north of the ITCZ, while Central and S. American dust prevails south of the ITCZ. In order to understand the nature of latitudinal and depth-related variations of mineral composition in terms of relative position to the ITCZ, deep-sea core sediments were collected from $9^{\circ}N$ to $17^{\circ}N$ at a $2^{\circ}N$ interval along the $131.5^{\circ}W$ meridian and analyzed for mineral composition. The amount of illite in surface sediments decreases gradually from 65% at $17^{\circ}N\;to\;31^{\circ}N$ to 31% at 9f. In contrast, smectite increases from 11% to 56% southward. The observed mineralogical variation toward the ITCZ is attributed to the increased supply of volcaniclastic material transported via the southeast trade winds from the Central and South America source regions. Smectite-illite transition, a phenomenon that the amount of smectite increases over illite, occurs at around $10^{\circ}N$, the northern margin of the ITCZ. This result indicates that the change in latitudinal position of the ITCZ in geologic past could be recorded as a form of smectite-illite transition in deep-sea cores. The studied cores show down-core variation of mineral composition from illite-rich at the surface to smectite-rich clay suit at depths, similar to the latitudinal variation. The smectite-illite transitions observed in these cores are likely the records of changes in latitudinal position of the ITCZ. The depth and age of smectite-illite transition is getting shallower and younger toward equator, implying that the ITCZ was located farther north during late Tertiary and has shifted southward to the present position of $5^{\circ}N-10^{\circ}N$.

• Proceedings of the KOR-BRONCHOESO Conference
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• 1991.06a
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• pp.28-28
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• 1991

후두암의 수직절제 수술후의 후두 재건 목적은 기관절개를 통하지 않고 후두를 통한 호흡이 가능하도록 하면서 연하시 기도흡인을 피하기 위한 sphincter 능력의 보존, 그리고 발성이 가능하도록 성대진동 mechanism을 재건하는데 있다. 오늘날 수많은 후두학자들에 의해서 고안 개발된 다양한 재건 방법이 있다. 연자는 광범위한 후두절제에 따른 큰 결손을 메우기 위해 bulky하면서도 점막 상피의 재생이 용이한 재건 피판으로 흉유돌근골막 피판을 이용하여 후두 결손부를 재건하여 보았다. 방법은 성견 3마리를 대상으로하여 thiopental sodium 정맥주사로 전신마취를 시행한 후 설골에서부터 흉골상까지 경부 정중앙의 피부를 절개하고 후두를 노출시켜 후두 수직절제술을 시행하였다. 흉유돌근과 흉골에 부착된 골막을 박리하여 흥유돌근골막 피판을 제작한 후 골막이 후두강 안쪽으로 되도록하여 골막연과 후두점막을 봉합하였다. 그리고 3, 5, 9개월에 후두적출술을 시행하여 병리조직학적 및 수술후 경과를 관찰하였다. 3실험견 모두 기관절개술 없이 후두를 통한 호흡이 가능하였고 흡입성 폐렴이나 피하기종등의 합병증없이 창상이 치유되었으며 발성도 양호하였다. 이식된 골막위로 신생혈관의 출현과 함께 점막재생이 잘되 있었다. 단지 봉합사 주위에 소량의 육아종이 관찰되었다. 조직학적으로는 섬유조직위로 편평상피가 재생되었으며 성문하부에서는 일부 섬모가 있는 호흡기 점막도 관찰되고 골막하부에 신생골 형성은 관찰할 수 없었다. 골막 피판은 그 유연성 때문에 결손부위의 점막연에 맞춰도 tension이 없고 공기 누출이 되지 않게 봉합이 가능할 뿐 아니라 점막이 재생할 수 있는 frame-work의 역할을 하는 것으로 사료되었다. 이상과 같은 사실로 미루어 흉유돌근 자체가 견실하고 골막에 혈류공급이 잘되어 창상치유에 좋을 뿐 아니라 큰 후두결손부의 재건이 가능하리라고 사료되었다.로서 몇가지 앞으로의 치료지침에 도움이 되는 결과를 얻었기에 보고하는 바이다. 1) 성별 분포는 남자 16(39 %), 여자 25 (61%)이었으며 1 : 1.5의 빈도를 보였다. 2) 연령 분포는 20대와 30대에서 남녀 모두 25명으로 대부분을 차지하였다. 3) 부식제의 종류는 빙초산이 26명 (63.4 %)으로 대부분을 차지하였고 염산 7 (17.1 %) Lye 3 (0.7 %) 의 순이었다. 4) 음독후 12시간내에 식도경술을 받은 환자가 3명(0.7 %) 12-24시간에 받은 환자가 17명(41.5 %), 24 - 48시간에 받은 환자가 11명(26. 8%)으로 48시간 내에 시행받은 환자가 전체의 75.6%를 차지하였다. 5) 식도경 검사상 나타난 식도화상은 Grade I 11명 (26.8%) G.ade II 18(43.9%) Grade III 7명(17.1%) 이었으며 Grade II 인 경우가 18명(43.9%)로 가장 많았으며 Grade I 11명(26.8 %), Grade III 7명 (17.1 %) Normal 5명 (12.2 %) 순이었다. 6) 조기 식도경 검사에서 41명중 oral cavity burn이 없었던 경우가 15명(36. 1 %) 이었으며, oral cavity burn이 있었던 26명중 5명(19 .2 %)에서 Esophageal burn이 없었다 특히 Esophageal burn의 Grade II, III 25명 중 9명(29.6 %)에서 oral cavity burn이 없었다. 7) 식도 부식중 환자의 치료 원칙으로 Grade I, II, III에서 항생제 및 보존적 치료를 하였으며 Grade I에선 oral feeding을 시켰고 Steroid는 경우에 따라 투여하였으며 Grade III에선 원칙적으로 사용치 않았다. 식도조영술은 Grade I II III에서 3주 후에 모두 시행하였다. 8) 3주 후 식도조영술을 실

• Journal of the Korean association of regional geographers
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• v.6 no.2
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• pp.71-82
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• 2000

The purpose of this paper is to clarify geomorphic features and development on the boulder stream of granitoid in Korea. Considering the purpose and the method of this paper, three boulder streams are selected : Biseulsan(Mt. Biseul) boulder stream (Daegu city), Maneosan (Mt. Maneo) boulder stream(Gyeongnam province), Geumjeongsan(Mt. Geumjeong) boulder stream (Busan city). The boulder streams mentioned above are bigger in scale and more typical in shape than any other ones in the Korean Peninsula. The main results are summarized as follows. 1. The following are the main features of the boulder streams morphology : the mean gradient is $3{\sim}25^{\circ}$, the longer axes of the component boulders within the deposits averaged about 2m in length, the shapes of the component boulders may be both subangular and subrounded features. 2. The formation of the component boulders is associated with deep weathering of granitoid under warm humid conditions, and the downward movement of boulders occurred by solifluction and frost creep under periglacial conditions. 3. The geomorphic development stage of the boulder streams may be classified into four stages. These boulder streams come under fossil landform stage, the 4th stage ; evidence provided by lichens and weathering features indicate inactive or fossil landform. 4. In generally, boulder streams are well developed on shallow valley floors.