http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
최석원,이남석,이재황,이현숙,채상정,Choi, Suck Won,Lee, Nam Seok,Lee, Jae Hwang,Lee, Hyun Sook,Cbae, Sang Jeong 국립문화재연구원 2001 헤리티지:역사와 과학 Vol.34 No.-
Paekche black potteries are earthenwares begun to be produced at the beginning of Paekche Dynasty, around 3-century. They have typical Paekche style. Representative Paekche earthenwares are burnished black pottery, long oval shaped pots and shoulder pots. Among these, burnished black potteries are limited to Paekche in the occurrence site and age. Their numbers are a few. To reproduce black pottery, their compositions were analyzed. As a result of X-Ray analysis, quarts, feldspar, illite, muscovite, and anorthite were found on their surfaces and imsides spinel and vermiculite were found on their surfaces. Since same constituent minerals were found on surfaces and their insides, special other materials were not added to make surface black. With the showing vermiculite, they were made higher than $800^{\circ}C$. As a result of analysis, fine grained clay bad been influenced by the black smoke. Its luster was appeared by polishing with a big flat wooden spoon. The black color was made of smoking when the hot pot taken off from burning oven was covered with the wet pine leaves.
폐쇄된 청계만에서 조간대 퇴적물의 퇴적환경과 지구화학적 특성
최석원 ( Choi,Suck-Won ),오강호 ( Kang Ho Oh ),정철환 ( Chull Hwan Chung ),윤석태 ( Seok Tai Youn ),김해경 ( Hai Gyoung Kim ),고영구 ( Yeong Koo Koh ) 한국도서(섬)학회 2010 韓國島嶼硏究 Vol.22 No.3
Considering the depositional environment and geochemical behaviors of metals, a total of 12 surface sediments were sampled along two sections in the tidal flats of Cheonggye bay. The mean size of sediments showed between -0.82Ø to 4.97Ø and 1.65Ø to 7.43Ø in Topmeori and Meoguri tidal flats and the sediments were sorted in 1.79Ø to 4.66Ø and 0.77Ø to 2.44Ø in above flats, respectively. The Topmeori flats are composed of msG, gM, gmS, zS and sM, while the Meoguri flats contained (g)S, zS, sZ, Z and M in facies. From the geochemical investigations of the sediments, major and minor elements of the sediments mostly showed the increasing trends toward open sea in contents. The elementary contents might be controlled by clay minerals produced from surrounding rocks, carbonate shell fragments, coarse feldspathic portions of the sediments related with circumferential geology and so forth. In addition, enrichment factors (EF) of the sediments were investigated. K, Mn, Ba, Li, Zn and Pb were enriched in the sediments. Of them, Li, Zn and Pb were generally related to organic contamination. Thus, administrations on above areas are needed in contamination.
경남(慶南) 함안(咸安)-군북지역(郡北地域)의 동광화작용(銅鑛化作用)에 관(關)한 연구(硏究)
박희인,최석원,장호완,채동현,Park, Hee-In,Choi, Suck-Won,Chang, Ho Wan,Chae, Dong-Hyeon 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.2
More than fifty copper veins are emplaced around late Cretaceous granitoid stock in Haman-Gunbuk district, southernmost part of Korea. These veins cut both late Cretaceous granitoids and hornfels of Jindong formation which is intruded by the granitoids. The paragenesis of veins is nearly the same, consisting of (1) an early vein stage in which most iron oxide minerals, tourmaline and other silitcate minerals were deposited, (2) a calcite and quartz with base·metal sulfide stage and (3) late vein lets of barren calcite stage. Fluid inclusion studies reveal highly systematic trends of salinity and temperature during mineralization. Ore fluids of early vein stage were complex NaCl-KCl rich brines. Salinities of polyphase inclusions in quartz and scapolite in thie stage reached up to 72 wt.% and gradually decreased to 10.5wt. % in closing stage. Homogenization temperatures of inclusions in the beginning of this stage were up to $490^{\circ}C$ and then declined steadly to $290^{\circ}C$ in the late stage. Salinities of fluid inclusions in quartz and calcite of base·metal sulfide stage were 37.4~5.7wt. % and homogenization temperatures range from $373^{\circ}C$ to $170^{\circ}C$. Intermittent boiling of early vein fluid is indicated by fluid inclusions in quartz. Potassic alteration of granodiorite adjacent to early vein seems to be related to early saline vein fluid. Fluid inclusion data of base-metal sulfide stage of this area reveal nearly the same range as those of Koseong copper mining district about 30km apart from this area.
다덕광산(多德鑛山) 풍정맥(楓井脈)의 금은광화작용(金銀鑛化作用)
박희인,최석원,이상선,Park, Hee-In,Choi, Suck-Won,Lee, Sang-Sun 대한자원환경지질학회 1988 자원환경지질 Vol.21 No.3
Ore deposits of Dadeok mine, the largest in the Bonghwa gold mining district, are composed of numerous gold and silver-bearing quartz veins emplaced in granite batholith. Mineralization of the Pungjeong vein, one of the representative vein in the mine was investigated. K-Ar age of sericite in the vein is $84{\pm}5$ Ma. Hypogene 6pen-space filling can be devided into four paragenetic stages; (1) fine grained quartz and carbonate; (2) quartz and carbonates with base metal sulfides, electrum, native silver, argentite, polybasite, freibergite, pyrargyrite, and Cu-Ag-Fe-S minerals; (3) quartz with base metal sulfides; (4) quartz and calcite with or without pyrite. Composition of electrum ranges from 44.17 to 56.50 atomic % Ag. Meanwhile FeS content of sphalerite coexisting with elctrum in stage II range from 0.01 to 1.67 mol. %. Homogenization temperatures for quartz and sphalerite of stage II ($239^{\circ}$ to $310^{\circ}C$), quartz of stage III ($206^{\circ}$ to $255^{\circ}C$) and quartz and calcite of stage IV ($232^{\circ}$ to $253^{\circ}C$) show little time-space variation during mineralization. Salinities of the fluid inclusions range from 5.5 to 12.8wt% NaCI in stage II, 7.3 to 12.3wt% in stage III and 4.5 to 8.0wt% in stage IV. Based on the homogenization temperatures, Fe content of sphalerite and Ag content of electrum, tempera ture and sulfur fugacity for stage II are estimated to be $208^{\circ}$ to $310^{\circ}C$ and $10^{-9.2}-10^{-12.8}$ bars, respectively.
대화(大華) 및 돈산(敦山) 중석(重石)·모리브덴 광상(鑛床)의 광석(鑛石)과 광물공생관계(鑛物共生關係)
박희인,최석원,김덕래,Park, Hee-In,Choi, Suck-Won,Kim, Deog-Lae 대한자원환경지질학회 1985 자원환경지질 Vol.18 No.1
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.
대화(大華) 중석휘수연광상산(重石輝水鉛床産) 광물중(鍵物中)의 유체포유물(流體包有物)에 관(關)한 연구(硏究)
박희인,최석원,Park, Hi In,Choi, Suck Won 대한자원환경지질학회 1974 자원환경지질 Vol.7 No.2
Daehwa tungsten-molybdenum deposits is fissure filled quartz veins occurring in Precambrian granite gneiss adjacent to the contact with Mesozoic biotite granite mass. Essential ore minerals are molybdenum and wolframite accompaning scheelite, cassiterite, chalcopyrite, pyrrhotite, pyrite and bismuthinites. Gangue minerals are quartz and little muscovte, fluorite, beryl and Carbonate minerals. Fluid inclusions in quartz, fluorite, beryl, scheelite and calcite have filling temperature ranges of $170-353^{\circ}C$. According to the studies of mineral paragenesis and filling temperature of fluid inclusion indicate that main tungsten and molybdnum mineralization have taken place with the minerals whose filling temperature ranges 205 to $353^{\circ}C$. Liquid $CO_2$ bearing fluid inclusions are characteristic in the quartz and early fluorite of tungsten and tungsten bearing molybdenum veins but hardly recognized from molybdemun veins. Estimated $CO_2$ concentration according to diagram proposed by the Takenouchi ranges from 10 to 20wt%. These facts suggest that tungsten mineralization may be related to the $CO_2$ content of the hydrothermal solution during the mineralizing period.