• Economic and Environmental Geology
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• v.26 no.3
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• pp.259-265
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• 1993

The variation of H/F coefficient (Hubnerite/Feberite coefficient) and the temperature of formation with depth have been studied for the hydrothermal tungsten-quartz veins from Ssangjeon, Weolag, Cheongyang, and Sannae mines. All samples were selected at the same paragenetic stage and mineral assemblege according to depth. The studied mines provide an opportunity to examine and regional variations in wolframite composition in different provinces. The formation temperature is linearly related to the depth. At the Weolag, Cheongyang and Sannae mines, the H/F ratio of wolframite and filling temperatures of fluid inclusions in quartz show a general tendency to decrease at shallow levels, in spite of different geological settings. This implies the pH of fluid will decrease vertically with falling temperature and the high H/F ratio of wolframite in deep zone result in an increase of pH with depth. The Ssangjeon mine exhibits a tendency to increase slightly upwards at shallow level. This implies a different geochemical environment (high pH environment) for the Ssangjeon mine, as compared to the other three mines. The H/F coefficient pattern suggests that it is a useful geothermometer for vein-type tungsten deposits in Korea. The H/F coefficient as an indication of depth should be examined for use in exploration.

• 보일러설비
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• s.21
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• pp.67-78
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• 1990

한반도에 사람이 살기 시작한 것은 구석기 시대의 유물이 한반도 각지에서 발굴됨에 따라 이 시대부터라는 것이 자명한 사실로 인정된다. 그러나 이들 구석기인들이 우리의 직접적인 조상이 된다고 할 수 없는데, 구석기 시대를 뒤이은 중석기 시대의 유적발굴과, 연구의 부족으로 중석기문화에 대한 단절이 있으며 신석기 문화가 새로 생겨났기 때문이다. 따라서 현 한국인의 조상으로부터 시작되는 한국주거사, 나아가 주택난방의 시작은 당연히 신석기 시대부터 고찰해야 할 것이다. 본고는 조선시대까지의 한국전통주택건축의 난방설계를 이해케하며 이를 통하여 한국전통 생활사의 일부를 밝힌 고려대학교 주남철 교수의 논고 $ulcorner$한국의 주택난방 변천과정$lrcorner$을 전재한 것이다.

• Mineral and Industry
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• v.26
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• pp.22-31
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• 2013

KIGAM and MRAM (Mineral Resources Authority of Mongolia) performed joint researches on geological survey of Dulaankhaikhan W-Mo occurrences areas in southeastern part of Khangai region. XRD results of tungsten containing quartz vein sample show that tungsten minerals are wolframite, hubnerite and ferberiteore. $WO_3$ grade of samples obtained in Silurian Khotont formation is 0.11-4.43% and that of samples obtained in Permian Delgerkhan complex is 137-3844 ppm. Average total $R_2O_3$ of samples obtained in survey area is 473 ppm which is 2.5 times larger than that of Earth's crust. The highest total $R_2O_3$ is 1326 ppm. Factor analysis results show that two areas of high tungsten contents have similar correlations with tungsten, and therefore we conclude that these two areas have the similar origin of mineralization.

• Proceedings of the KSEEG Conference
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• 2003.04a
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• pp.209-212
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• 2003

한국의 금속광산은 일제시대에 금광산을 중심으로 본격적으로 개발되어 1943년 산금령시에 1,522개 광산이 가행되었다. 최근까지 1990개 광산이 개발된 것으로 알려지고 있으며 2002년 말 현재 7개 광산만이 가행되었다. 1960년대까지 국내 광산은 금, 은 동, 연아연, 철, 중석 등을 중심으로 활발히 가행되어 주요 외화 획득원으로 중요한 위치를 차지하였다. 그 이후 산업발전에 따라 수요는 증가세를 보인 반면 가행광산과 생산량은 매년 감소하여 최근 금속광물자원 자급도는 0.21%로 미미한 수준이며 수요의 대부분을 해외에 의존하고 있다. (중략)

• Economic and Environmental Geology
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• v.20 no.3
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• pp.179-196
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• 1987

Various skarn ore deposits of Pb-Zn, Fe-Cu, W-Mo and others are widely distributed in the study area which consists mainly of Cambro Ordovician calcareous rocks. The ore deposits are all in close association with specific types of granitic rocks of mid-late Cretaceous age according to the kinds of ores: Fe-Cu deposit with granodiorite-quartz monzodiorite, Pb-Zn deposit with granite-granodiorite, W-Mo deposit with granite, and Mn deposit with quartz porphyry. The granitic rock of Fe-Cu deposit has lower content in K and higher in Ca than those of Pb-Zn deposits. On the contrary, the granitic rock of W-Mo deposit has much higher content in K and lower in Ca in comparison to those of Pb-Zn deposits. However, the granitic rock of Mn deposit shows similar variation to those of Pb-Zn deposits. Lithophile trace elements of Sr and Rb tend to vary in close relation with major elements of K and Ca, respectively. In good contrast, chalcophile elements of Cu, Pb, Zn, Wand Mo are enriched in the granitic rocks of their ore deposits, and other trace elements of Ni and Co show a trend to vary in relation with Mg, Fe and Cu, which have the same replacement index (0.14) as Ni and Co. Average K/Rb and Ca/Sr ratios of the granitic rocks range nearly within 300~150 and 150~40, respectively, and the distribution pattern of the ratios is different according to the kind of ore deposits: Fe-Cu deposit is plotted toward K-Rb poor region whereas Pb-Zn and W-Mo deposits toward K-Rb rich region. In contrast, Fe-Cu and Fe deposits are plotted toward Ca-Sr rich region whereas Pb-Zn deposit toward Ca-Sr poor region. The variation trend of chemical elements of the mid-late Cretaceous granitic rocks in the study area is similar to that of the Cretaceous granitic rocks in the Gyeongsang Basin. Therefore, this geochemical result may be applicable to determining what kinds of ore deposits a Cretaceous granitic rock is favourable for, and whether it is productive or non-productive for systematic geochemical exploration works.

• Proceedings of the Korea Society for Simulation Conference
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• 2002.05a
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• pp.189-195
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• 2002

궤도차량 운동의 실시간 시뮬레이션을 위해서 실시간 시간제약 조건을 만족하기 위한 모델링을 시도하였다. 단위 블록 열차로 연결된 전체 차체를 질점으로 가정하여 모델을 단순화함으로써 차량 설계 시 사용되는 궤도 차량 모델보다 실시간성을 향상시키고자 하였다. 당 모델에서 궤도차량의 운동은 트랙의 형상에 구속되는데, 차량의 운동 궤적은 궤도의 형상에 의해 결정된다. 단, 매 단위 시간마다에서 궤도 차량의 위치는 뉴턴의 제2법칙으로 결정된다. 본 모델링은 몇 개의 단위 트랙을 설정하여 이들의 조합으로 전체트랙을 설계할 수 있도록 사용자가 임의로 설계한 전체트랙에서 바로 실시간으로 시뮬레이션할 수 있는 특징을 갖는다. 당 궤도차량 운동 모델은 전동차, 철도, 롤러코스터의 궤도 설계 등에 사용될 수 있으며, 주 용도는 롤러코스터 게임 시뮬레이터에서 동 특성을 비교적 엄밀하게 시뮬레이션 하는데 있다.

• Journal of the korean Society of Automotive Engineers
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• v.15 no.4
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• pp.1-7
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• 1993

최근 엔진의 고성능, 고출력화, 저연비화 Maintenance Free화에 따라 엔진의 부하가 증대되었고, Valve Seat에 대해서도 내마모성, 내열성, 내식성 향상이 요구되고 있다. 특히 무연가솔린과 LPG사용으로 내구성을 갖는 High Performance의 Valve Seat 재질을 요구하게 되었고, 엔진의 높은 작동온도등 가혹한 조건하에서 'Recession'이라 일컬어지는 Seat마모가 생기게 된다. Valve Seat는 일반적으로 분말야금법에 따라 제조되고 있으며, 엔진조건에 따라 여러가지의 재질이 사용되며, 높은 온도에서 열전도성과 기공의 산화방지 및 Valve 내구성 향상의 효과를 얻기 위하여 동용침을 하여 사용하는 추세이다. 본 실험에서는 Valve Seat 기공부위의 산화와 마모특성을 조사하기로 한다.

• Journal of the Mineralogical Society of Korea
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• v.20 no.4
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• pp.231-245
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• 2007

The forged iron axe of the middle 3rd Century found in the No. 2 wood-framed tomb from the Hwangseongdong site, Gyeongju is rectangular on the plane level. The iron axe shines in met-allic luster, which is light grey with pale creamy tint. The result of X-ray diffraction analysis shows that the axe consists of magnetite and geothite, which can explain why the composition and texture of the original ore has been kept intact. There are fine-grained quartz, calcite, mica, magnetite, amphibole, unknown tungsten minerals, pyroxene and olivine inside the axe. Those must be the impurities that they failed to remove in the thermal treatment process. Generally, the iron axe consists mainly of pearlite texture coexisting ferrite and cementite, and show high carbon contents with homogeneous distribution. It can be interpreted the axe was carburized after the material was made to resemble pure iron. The decarbonization work didn't go well along the process marks. Crude ores of the iron axe are possible utilized by magnetite from the Ulsan mine on the basis of the occurrences and inclusions. It's estimated that the original ore was bloom produced in low-temperature reduction and formed around in $727^{\circ}C$, which is eutetic temperature.

• Economic and Environmental Geology
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• v.13 no.2
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• pp.104-116
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• 1980

The Ulsan mine is one of the largest contact metasomatic magnetite and scheelite deposits in the southeastern part of Korea. Mineralization at the Ulsan mine is localized along the contact between upper Cretaceous volcanic rocks and age unknown limestone which were intruded by 58 m.y. -old biotite-horndlende granite. General zonal sequence of skarn toward crystalline limestone from limestone-volcanics contact is grandite, grandite-salite and salite zones. On the otherhand volcanics origin skarns exhibits zonal sequences toward hornfels from boundary with limestone is garnet, garnet-epidote, and epidote zone. Compositions of garnets and clinopyro xenes are determined by the X-ray diffraction and reflective indecies. Local brecciation of these early skarns were followed by formation of the later skarn as zoned patches, breccia fillings and cross-cutting veins. Paragenetic sequence of late skarn minerals which is exhibited in the zoned patches and veins is an overlapping progression with time from andradite through hedenbergite or actinolite, quartz to calcite deposition. Magnetite metallization followed early formed skarns and pyrite pyrrhoite, sphalerite, galena, tennantite, scheelite and arsenopyrite deposition were simultaneously with hedenbergite, quartz and calcite of late skarn. Filling temperatures of fluid inclusions in calcites range from $160^{\circ}$ to $280^{\circ}C$.

• Mineral and Industry
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• v.28
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• pp.1-13
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• 2015

In this study, it was carried out separation process research and development to be able to produce high-grade tungsten concentrate form tungsten taken form Mongolia. In order to reduce treatment cost and increase separation efficiency the jig separation at first was applied for recovering the concentrate. Which reground would make the degree of liberation increase. Which was treated by shaking table to reject the gangue minerals from the first concentrate. Because the heavier product contains not only ferberite but also cassiterite, the product was treated by further dry magnetic separation to obtain the ferberite concentrate. Finally, the high-grade ferberite concentrate of 67.63% $WO_3$ could be obtained with recovery of 86.07% through the separation process developed in this study.