• 자원환경지질
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• 제27권4호
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• pp.325-333
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• 1994

Gold and/or silver mineralization in the southeast province, Korea, occurred in hydrothermal quartz vein that fills fracture zones in Cretaceous volcanic and sedimentary rocks of the Gyeongsang basin or granites and Precambrian gneiss. Most of the gold-silver-bearing veins in the province occur in Hapcheon, Suncheon and Haman-Gunbuk area where they are associated with Cretaceous Bulgugsa granites. On the basis of the Ag/Au ratio on amounts produced and ore grades, mode of occurrence, and associated mineral assemblages, hydrothermal Au-Ag deposits in southeast province, Korea, can be classified as follows: pyrite-type gold deposit (Group IIB, Samjeong and Sangchon deposits), antimony-type gold-silver deposit (Group IV, Gisan and Geochang deposits), and antimony-type silver deposit (Group V, Sanggo, Seweon, Seongju and Gahoe deposits). All of the gold-silver deposits in the province are generally characteristics of the gold-silver or silver-dominant type deposit which contains more silver-bearing minerals than those deposits in central Korea. The gold-silver mineralization in the deposits consist of two generation; the early characterized by gold precipitation and the late represented by silver-rich (as silver-bearing sulfosalts minerals) mineralization. All but one deposit (Samjeong deposit) having relatively lower Au content in electrum values between ${\approx}20$ and ${\approx}50$ atomic %. The mineralogical data on electrum-sphalerite and/or arsenopyrite geothermometry and fluid inclusion data indicate that the gold and silver mineralizations were occurred at temperatures of $190{\sim}280^{\circ}C$ and $150{\sim}180^{\circ}C$, respectively. These suggest that the gold-silver mineralization in the province occurred in the lower temperature and pressure conditions as epithermal-type hydrothermal vein deposit.

• 자원환경지질
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• 제21권3호
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• pp.223-234
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• 1988

A large number of gold and/or silver-bearing quartz veins occur in or near Mesozoic granite batholith elongated in a NE-SW direction within the Chungcheong Province. Precambrian schists and gneisses, and Jurassic and Cretaceous granitic rocks serve as hosts for gold and/or silver deposits. On the basis of Ag/Au total production and ore grade ratio, 15 mines may be divided into three major groups: gold-dominant deposits, gold-silver deposits, and silver-dominant deposits. The chemical composition of electrum from skarn deposit (Geodo mine), alaskite-type deposit (Geumjeong mine) and 15 vein deposits was summarized. It was found that the Au content of electrum for vein deposits ranging from 5.2 to 86.5 is lower than that for skarn and alaskite deposits. Among 15 vein deposits, the composition of electrum associated with pyrrhotite is relatively high and has a narrow range of 40.8 to 86.5 atomic % Au, but the Au content of electrum with pyrite is in range of 5.2 to 82.8 atomic %, and is clearly lower than that with pyrrhotite. The grouping of ages for these mines indicates that gold and/or silver mineralizations occurred during two periods in the Mesozoic. Daebo igneous activities are restricted to gold mineralization in the range of 158 to 133 Ma, whereas Bulgugsa igneous activities are related to gold and/or silver mineralization ranging from 108 to 71 Ma. Generally speaking, Jurassic gold-dominant veins have many common characteristics; notably prominent association with pegmatites, simply massive vein morphology, high fineness in the ore concentrates, rarity of silver minerals, and a distinctively simple mineralogy, including sphalerite, galena, chalcopyrite, pyrrhotite and/or pyrite. Although individual deposits exhibit widely differing diversity, Cretaceous gold-silver and silver-dominant veins are characterized by features such as complex vein, low to medium fineness in the ore concentrates and abundance of silver minerals including Ag sulfosalts, Ag sulfides, Ag tellurides and native silver.

• 대한자원환경지질학회:학술대회논문집
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• 대한자원환경지질학회 2001년도 춘계 공동학술발표회
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• pp.252-252
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• 2001

• 한국분말재료학회지
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• 제14권3호
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• pp.165-172
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• 2007

The purpose of this study was to analyze the sintering characteristics of gold and silver nanoparticles. In this study, gold and silver nanoparticles were prepared by using Inert Gas Cndensation (IGC). The sintering temperatures for gold and silver nanoparticles were $100{\sim}1000^{\circ}C\;and\'100{\sim}500^{\circ}C$, respectively. The sintering characteristics of gold and silver nanoparticles prepared by IGC were evaluated by X-ray diffraction(XRD), transmission electron microscopy (TEM), and scanning electron microscopy (SEM). Gold and silver nanoparticles with the size of $1{\sim}100\;nm\;and\;10{\sim}100\;nm$, respectively, were obtained. The size of sintered gold and silver nanoparticles increased with an increase in the sintering temperature. XRD data showed that silver nanoparticles were similar with polycrystal single-phase.

• 자원환경지질
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• 제21권4호
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• pp.367-380
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• 1988

Most of the gold (-silver) vein deposits at Yeongdong District are mainly distributed in the precambrian metamorphic rocks. Based on the Ag/Au total production and ore grade ratios, the chemical composition of electrum and the associated sulfides, the gold(-silver) deposits at Yeongdong District may be classified into 4 classes: pyrrhotite - type gold deposits( I), pyrite - type gold deposits (IT A; massive vein), pyrite - type gold deposits (II B; nonmassive vein) and argentite - type gold - silver deposits(III). The chemical study on electrum(including native gold) revealed that Au content (2.8 to 92.4 atomic%) of electrums varies very widely for different classes of deposits. The Au content of electrum associated with pyrrhotite (Class I), ranging from 47.1 to 92.4 atomic% Au, is clearly higher than that associated with pyrite (Classes IIA, IIB and III). In contrast, classes I, II, and III deposits do not show clear differences in Au content of electrum. In general, pyrrhotite - type gold deposits(I) are characterized by features such as simply massive vein morphology, low values in the Ag/Au total production and ore grade ratios, the absence or rarity of silver - bearing minerals except electrum, and distinctively simple mineralogy. Although the geological and mineralogical features and vein morphology of pyrite - type gold deposits(IIA)are very similar to those of pyrrhotite - type gold deposits (I), Class II A deposits reveal significant differences in the associated iron sulfide (i. e. pyrite) with electrum and Au content of electrum. The Ag/Au total production and ore grade ratios from Class II A deposits are relatively slightly higher than those from Class I deposits. Pyrite - type gold deposits(II B) and argentite - type gold - silver deposits (III) have many common features; complex vein morphology, medium to high values in the Ag/Au total production and ore grade ratios and the associated iron sulfide (i. e. pyrite). In contrast to Class II B deposits, Class III deposits have significantly high Ag/Au total production and ore grade ratios. It indicates distinct difference in the abundance of silver minerals (i. e. native silver and argentite). The fluid inclusion analyses and mineralogical data of electrum tarnish method indicate that the gold mineralization of Classes I and II A deposits was deposited at temperatures between $230^{\circ}$ and $370^{\circ}C$, whereas the gold (-silver) mineralization of Classes ITB and ill formed from the temperature range of $150^{\circ}-290^{\circ}C$. Therefore, Classes I and IT A deposits have been formed at higher temperature condition and/or deeper positions than Classes IIB and III.

• 대한한의학원전학회지
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• 제37권3호
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• pp.1-9
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• 2024

Objectives : This study aims to clarify the interpretation of the verse "jinyinhuabohetangxia(金銀花薄荷湯下)" in Zhouxuehai(周學海)'s corrective commentary in the Xiaoeryaozhenzhijue(小兒藥證直訣), by examining traditional pediatric texts in relation to the verse. Methods : For each of the three possible interpretations of the instructive phrase for taking herbal formulas-Lonicera flower with peppermint(金銀花+薄荷), gold and silver with peppermint(金銀+薄荷), and gold coin peppermint(金錢薄荷)-applications of these herbs in the various pediatric books were analyzed to determine the most appropriate interpretation. Results & Conclusions : The formulary composition of Liangjingwan(凉驚丸) and Wusewan(五色丸) seems to sufficiently target the pathology of pediatric convulsion(驚癎) and heart malnutrition(心疳). Furthermore, it seems unnecessary to add Lonicera flower(金銀花) to the gastrointestinal fragility(脾胃虛弱) of the malnourished(疳). Some of the herbal formulas in the pediatrics chapter of the Zhengzhizhunsheng(證治准繩) include Lonicera flower(金銀花) to treat only carbuncles(癰腫, 腫毒), while other books do not include it in their formulas. On the other hand, instructions to take water boiled with gold and silver appear in many texts, including the Xiaoeryaozhenzhijue(小兒藥證直訣), and sometimes include gold leaf(金箔) directly in the formula. Descriptions of gold and silver pots with instructions on how to make herbal formulas were found as well, which supports what Zhouxuehai(周學海) commented on the Xiaoeryaozhenzhijue(小兒藥證直訣). Although gold coin peppermint(金錢薄荷) is currently used as Lianqiancao(連錢草) in China, it was difficult to verify its identity as Jinqianbohe(金錢薄荷), which seems to have been recognized as a type of mint in the past. No reported anticonvulsant studies of Lonicera flower(金銀花), gold and silver(金銀), and Lianqiancao(連錢草) were found. Peppermint(薄荷) was ubiquitous in instructions for taking herbal formulas treating pediatric convulsions. Therefore, the instruction to take water boiled with gold and silver, or to take the herbal medicine in water boiled in a gold and silver pot, rather than using Lonicera flower(金銀花), could be considered as an interpretation closer to the original author's intent.

• 한국광물학회지
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• 제21권4호
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• pp.383-395
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• 2008

필리핀 만카얀 지역의 빅토리아 광산에서 입수한 금 은 광석으로부터 금 은 성분의 회수율을 높이기 위해 지질 및 광물학적 특성, 금과 은의 수반상태, 파 분쇄에 따른 단체 분리도, 체 분리에 의한 분립 특성과 요동테이블에 의한 비중 선별 특성을 연구하였다. 필리핀산 금 은 광석은 황철석, 섬아연석, 방연석 등의 황화광물과 석영 및 점토 등의 맥석 광물로 구성되었다. 금 은 성분은 황철석, 섬아연석, 방연석 등의 황화광물에 주로 수반되어 있었다. 황화광물 결정의 크기는 $100{\mu}m$에서 $1{\mu}m$ 이하까지 광범위한 입도분포를 갖기 때문에 금 은이 수반된 황화광물의 단체분리도를 높이기 위해서는 금 은 광석을 최소한 $100{\mu}m$ 이하로 매우 작게 분쇄해야 하는 것으로 나타났다. 금 은 광석을 Jaw crusher $\to$ cone crusher $\to$ rod mill 등으로 단계적으로 파.분쇄하여 입도($d_{90}$)를 $100{\mu}m$ 이하로 조절하면 단체분리도가 92% 정도까지 높아졌다. 금 은 성분이 함유된 황화광물의 결정이 $100{\mu}m$ 이하의 입단에서 고르게 분포되어 있기 때문에 체질에 의한 분립 방법으로는 금 은을 수반한 황화광물을 선택적으로 분리하여 회수할 수 없었다. 파 분쇄한 금 은 광석을 체로 분립한 후 요동테이블로 비중 선별한 결과, 정광에는 황화광물이 주로 농축되어 금과 은의 품위가 각각 40 ppm 및 140 ppm까지 높아졌다. 이때 정광의 금 실수율은 거의 100%에 이르지만, 은 실수율은 50% 수준에 불과하였다.

• 자원환경지질
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• 제21권3호
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• pp.287-307
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• 1988

The Cheongju gold-silver mine is located at approximately $36^{\circ}28^{\prime}$north latitude and $127^{\circ}31^{\prime}$ east longitude in the Cheongju City of the Chung cheong bug Do, South Korea. Gold-Silver bearing hydrothermal quartz veins, occur in Cheongju Granit of Jurassic age. K-Ar isotope data for sericite in quartz vein indicate that the Au-Ag mineralization took place in early Cretaceous ($97.5{\pm}2.18$ MA. Park, et ai, 1986). Three stage of mineralization recognized anre, from early to later, (I) Sulide stage: pyrite, arsenopyrite, pyrrhotite (Hpo), sphalerite, chalcopyrite, electrum and quartz (II) Electrum stage: pyrite, sphalerite, galena, chalcopyrite, electrum and quartz. (III) Silver mineral stage: pyrite, marcasite, pyrrhotite (Mpo), sphalerite, galena, electrum, native silver argentite, fluorite, calcite and quartz. In this paper, mode of occurrences and chemical compositions of electum and native silver have been investigated by means of microscope and EPMA. Electron probe microanalysis shows that an individual grain of electrum is almost homogeneous in composition. Silver content of electrum ranges from 44.7-67.1 atom.%. Gold content of native silver ranges below 0.2 atom. %. Vicker's hardness number (VHN) of electrum and native silver ranges $78.2-81.8kg/mm^{2}$ respectively. The filling temperature of fluid inclusions in quartz ranges from $130-280^{\circ}C$. On the basis of arsenpyrite geothemometer, the equilibrium temperature and sulfur fugacity of the pyrite-arsenopyrite-pyrrhotite(Hpo) assemblage is assumed to be in ange from $300-310^{\circ}C$ and $10^{-10}$ to $10^{-11}$ atm. The estimated ore reserviors on Cheongju mine area are calculated to 8000 T/M, averaing 8.6g/t Au, 27.8 g/t Ag, 1.25% Pb, l.65% Zn.

• 자원리싸이클링
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• 제10권1호
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• pp.42-48
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• 2001

The dissolution behavior of gold and silver from gold-silver alloys in aerated cyanide solutions has been investigated by an electrochemical means as well as a direct measurement of gold and silver ions reported in the bulk solution as a function of time using rotating disc electrodes. The variables studied included oxygen partial pressure, rotating speed of the disc, concentration of cyanide, temperature and composition of the allyos. The dissolution potential and the rate of dissolution were obtained in view of the anodic and cathodic current-potential relationships. The results were discussed in terms of the mixed potential theory. The results showed that the dissolution rate of gold and silver from the alloys was controlled partially by chemical reaction. but largely by transport of either oxygen or cyanide, depending on their relative concentration under the experimental conditions employed in this study.

• 자원리싸이클링
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• 제26권5호
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• pp.3-11
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• 2017

금과 은은 귀금속으로 첨단소재를 제조하는데 사용된다. 용매추출은 다양한 침출용액으로 부터 순수한 금과 은을 회수할 수 있는 중요한 공정이다. 본 논문에서는 cyanide, thiocyanate, thiosulfate, thiourea과 염산용액에서 금(I, III)과 은(I)의 용액화학 및 용매추출에 의한 분리를 고찰했다. 여러 단독 및 혼합추출제에 의한 금(I, III)과 은(I)의 용매추출 및 분리거동을 각 침출용액에서 추출반응과 추출제의 선택도를 토대로 비교했다. 염산용액이 용매추출에 의한 금과 은의 분리의 효율측면에서 적당하다.