• 기술사
• /
• 제3권10호
• /
• pp.3-6
• /
• 1970

The scheelite occurred in Sang Dong mine are disseminated with a fine grain, and shelved pale blue or white color under the fluorescence. But among them, We can often observe the yellow fluorescent color mineral grains, which were called the powellite from the past time without any detail mineral study. I studied the characteristics of Sang-Dong scheelite and the so called powellite. In the result, the so called powellite is proved to be the molybdenum bearing scheelite in the view of specific gravity, index of refraction, chemical composition, other microscopic properties, and dressing. Such a scheelite is contained usually Zor 3% Mo, and oftenly 4 or 6% Mo, and fluorescent colors are pale yellow, leman yellow and chrome yellow.

• 자원환경지질
• /
• 제12권4호
• /
• pp.197-206
• /
• 1979

Sangdong scheelite deposit is confirmed to have been formed by replacement of limestone beds by metasomatic mineralization. Mineralogical zonal distribution and filling temperatures are related with order of its formation and tungsten mineralization. The first formed garnet-pyroxene zone, left in the margins of the ore body, shows the highest filling temperature of fluid inclusions in pyroxene, averaging $420^{\circ}C$. The central part of the ore body, mainly composed of quartz-mica-scheelite, shows higher fi11ing temperatures of fluid inclusions in quartz, than hornblende-quartz-scheelite zone surrounding the quartz-mica-scheelite zone, averaging $240^{\circ}C$. The distribution of highter filling temperatures above average temperature is applicable to the richest part of scheelite distribution. Generally scheelite shows higher filling temperature by about 20 to $100^{\circ}C$ than quartz in a given sample. The crystallization temperature of the main phase of scheelite deposition is $311^{\circ}C$ at the pressure of 230 to 500 bars at Sangdong area. Gas-rich inclusions in the pyroxene are homogenized into either gas or liquid phase or into both phases in a given crystal of the pyroxene, which suggests boiling at the formation of skarn.

• 자원환경지질
• /
• 제13권2호
• /
• pp.117-127
• /
• 1980

Molybdenum as by-products of Sangdong tungsten mine occurrs in the form of molybdenite in quartz vein. The molybdenum contents of scheelite in Sangdong ore bodies ranges from trace to 8%, therefore the scheelites show variable fluorescence colores under ultra-violet lamp (short wave). The fluorescence color are in order high content of molybdenum, yellow, white and blue. The yellow fluorescing scheelite is dominant in upper ore vein, otherwise the blue fluorescent variety is dominant in lower ore vein. The fluorescence color of scheelite in the main ore vein show zonal distribution becoming progressively more blue outerwards, contrary more yellow innerwards, and even in single scheelite crystal, simillar zonal pattern is observed, too. Molybdenite occurrs as flakes or elongated blades at the margins of the quartz vein only molybdenite bearing quartz veins but also other sulfides mineral bearing quartz veins have mainly blue flourescing scheelites. We suggest that the molybdenum contents of the early stage ore solution are progressively decreased by a subsequent crystallization of the yellow fluorescing scheelites.

• 자원환경지질
• /
• 제11권4호
• /
• pp.143-167
• /
• 1978

The Sangdong tungsten (mostly scheelite) mine is located on the southern limb of a major syncline, the Hambaeg syncline, in a thick sequence of lower Paleozoic sedimentary rocks in the mideastern part of south Korea. Productive scheelite mineralization in Sangdong area is confined to one single formation, the Myobong Slate. Four major ore beds, which have an lateral extension over than 1 km and were not heavily subjected to spatial disturbance, are developed in the Myobong Formation. The original materials of the ore-comprising horizones were probably of either calcareous or silceous sediments. The four ore beds, especially in the case of Main ore bed, display both lateral and vertical zoning. Association quartz-mica-scheelite is predominant in the central, while association hornblende-quartz-diopside-scheelite, diopside-garnet and wollastonite-garnet are developed in this order towards the periphery of the ore beds. Petrologically, two phases of thermometamorphism are recognized. The first phase is represented by the association wollastonite-garnet and diopside-garnet, while the second phase by the association hornblende-quartz-diopside-scheelite and quartz-mica-scheelite. The associations of the second phase do constitute prodctive ore. The high background value of tungsten in the area surrounding the Sangdong mine reveals that the area can be considered a geochemical zone enriched in tungsten. Studies on the trace element patterns were carried out to draw useful criteria for the purpose of future geochemical exploration in the area. The increasing trend of the ratio Rb $({\times}1000)/K_2O$ of the Myobong Slate towards the known mineralization area proved to be indicative for the presence of tungsten mineralization.

• 공업화학
• /
• 제4권3호
• /
• pp.591-600
• /
• 1993

염소화에 의한 텅스텐 추출 공정의 공업화를 위해 유동층 반응기에서 회중석의 염소화반응이 조사되었다. 본 실험의 모든 결과는 텅스텐 성분이 유동충 반응기에서 성공적으로 염소화됨을 보여주었다. 본 실험의 적정 조건은 다음과 같다. : 반응온도 $900^{\circ}C$, 반응시간 : 20 min, 염소가스 유속 : 13.2cm/sec 그리고 회중석에 대한 petroleum coke의 무게비 : 0.2 또한 회중석과 petroleum coke의 평균 직경은 각각 $150.5{{\mu}m}$ 그리고 $750.9{{\mu}m}$이다. 이러한 조건하에서 회중석 중의 텅스텐 성분이 95% 이상이 염소화되었다.

• 자원리싸이클링
• /
• 제13권3호
• /
• pp.19-26
• /
• 2004

회중석 광석의 부유선별 공정에서 발생된 폐광미를 보통포틀랜드시멘트의 원료로 이용하기 위하여 폐광미의 사용량에 따른 조합원료 및 시멘트 클링커의 특성을 연구하였다. 폐광미에는 68.8%의 $_2$, 8.6%의 $Al_2$$O_3$, 10.8%의 Fe$_2$$O_3$, 5.0%의 CaO가 함유되어 있고, 주로 $\alpha$-quartz, muscovite, clinochlore 등으로 존재하며, 88$mu extrm{m}$ 잔사가 약 8.0% 정도 이다. 석회석, 전로슬래그, 플라이애쉬, 폐광미 등의 조합원료를 LSF: 91.0, SM: 2.60, IM: 1.60의 modulus로 혼합하여 클링커를 합성한 결과, 조합원료의 소성지수는 50.7정도이고, 클링커에 함유된 $C_3$S 및 $\beta$-C$_2$S의 결정크기는 15∼35$\mu\textrm{m}$로, 폐광미를 조합원료에 약 3.8%까지 사용할 수 있었다.

• 대한화학회지
• /
• 제7권1호
• /
• pp.17-24
• /
• 1963

本硏究에서는 韓國産 灰重石($CaWO_4$)에 關하여 固相一液相界面에 있어서의 電氣化學的 性質을 電氣泳動法으로 調査하고 한便 浮遊性에 關하여서는 捕收劑로 Dodecyl ammonium chloride(D.A.C.라 略稱)와 Sodium dodecyl sulfate(S.D.S.라 略稱)를 使用하여 Hallimond tube 試驗, 接觸角測定 及 吸着量測定等의 捕收劑 이온이 鑛物表面에 吸着하는데 있어서 電氣的인 相互作用이 重要한 役割을 하고 있다는 것을 實證하였다. 卽 電氣泳動法으로 鑛粒의 水溶液中에 있어서의 mobility를 測定한 結果 灰重石의 境遇에는 $Ca^{++}$ 或은 $WO_4^{--}$이 界面 電氣特性을 決定하는 potental determining ion이라는 것이 確認되었고 水溶液中에 있는 $Ca^{++}$의 增加는 鑛粒界面의 陰電荷를 減少하며 $WO_4^{--}$의 增加는 그 陰電荷를 增加한다는 것을 알수 있다. 이와같은 表面에 "陰이온系"의 S.D.S. 或은 "陽이온系"의 D.A.C.를 作用시키면 當然히 S.D.S.는 $Ca^{++}$의 增加에 따라 吸着量이 增加되어 浮遊性이 增大되고 한便 D.A.C. 때는 反對로 $WO_4^{--}$이 增加하는데 따라 吸着量이 增加되며 따라서 浮遊性도 增大된다고 불수 있고 實地로 捕收劑吸着量의 測定 및 Hallimond tube 實驗은 이것을 立證하고 있다. 이러한 基礎的인 究明은 灰重石浮選理論의 根幹이 되는 것이고 從來의 浮選法 改良에 對한 指針이 될수 있다고 生覺한다.

• 공업화학
• /
• 제4권1호
• /
• pp.82-93
• /
• 1993

염소화 공정을 통해 batch-boat-system에서 회중석으로부터 텅스텐 성분을 추출하기 위해, 환원제인 탄소의 무게비, 반응온도, 반응시간, $Cl_2$ gas의 유량 그리고 시료입도와 같은 주요 반응 변수들에 대한 영향을 조사하였다. 이 염소화 공정들에 대한 적정조건들은 반응온도 $700^{\circ}C$ 이상, 광물시료에 대한 탄소의 무게비 0.08, 반응시간 20분, $Cl_2$ gas의 유량 $0.6{\ell}/min$, 광물시료의 입도 -200mesh였으며 위 조건하에서 광물중 99%의 tungsten성분이 추출되었다. 반응속도는 고온에서는 $Cl_2$ gas의 확산단계가, 저온에서는 화학반응단계가 속도결정단계로 보이며 각각의 단계에서 활성화 에너지는 고온 부분에서는 7.98kcal/mol이며 저온 부분에서는 31.2kcal/mol이었다.

• 자원환경지질
• /
• 제2권2호
• /
• pp.73-75
• /
• 1969

Ogbang scheelite deposit imbedded in amphibolite of unknown age was believed, by the previous workers, to be of pegmatite vein. The vein material is composed mainly of plagioclase (albite and oligoclase) and minor amount (less than 5 to 10% each) of hornblende, biotite and quartz. Orthoclose and tourmaline are accompanied in few places and scheelite and minor amount of fluorite, are the ore minerals. On the basis of mineralogical constituents of the vein, vein structures, mode of occurrence of the vein and gradational contact between veins and amphibolite, the present writer conclude that the deposit was formed by segregation from the parent basic igneous rock of amphibolite. The main portions of the deposit were formed by intrusion of ore solution into already solidified amphibolite after being segregated in deeper horizone, whereas the minor portion by segregation of ore solution in situ.

• 자원환경지질
• /
• 제16권1호
• /
• pp.37-49
• /
• 1983

The skarn type tungsten deposits are developed in the contact aureole of Jurassic biotite-hornblende granodiorite and limestone beds. The latter can be divided into the Great Limestone Series of Joseon System and Gabsan Formation which is correlative to the Hongjeom Series of Pyeongahn System. The skarns are impregnated in the limestone, sandstone, schist and granodiorite, and showing zonal distribution. The five skarn zones are from fresh limestone inwards to wollastonite-skarn, clinopyroxene-skarn, clinopyroxene-garnet skarn, garnet skarn and vesuvianite skarn zone. The ore mineral, scheelite, disseminates in the clinopyroxene-garnet and vesuvianite skarn zone, and the size of the scheelite crystals in vesuvianite skarn zone is larger than in clinopyroxene- garnet skarn zone. According to the mineral paragenesis and the composition of skarn minerals, oxygen fugacity ($fo_2$) is low. Fluid inclusions in quartz comprise much $LCO_2$ and fluid inclusion studies revealed that the homogenization temperatures range $240-290^{\circ}C$.