• 자원리싸이클링
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• 제32권6호
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• pp.34-44
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• 2023

본 연구에서 고품위 몰리브데나이트 정광회수를 위해 요인설계를 이용한 컬럼부유선별을 수행하였다. 먼저 삼양 마이닝 플랜트의 부유선별 정광의 단체분리 향상을 위해 평균 입도 165, 116, 46.7 및 38.4 ㎛로 각각 재분쇄하였다. 컬럼부선에 영향을 미치는 다양한 변수에 대한 실험을 수행하였으며 MoS₂ 품위와 회수율이 각각 98.3 %와 95.28 %인 정광을 얻었다. 또한, 고품위에 영향을 미치는 입도 크기, 세척수 속도 및 억제제에 관한 요인설계 및 실험 데이터를 확보하고 통계분석(SPSS 25) 프로그램을 이용해 회귀분석하였다. 결과로부터, 컬럼부선 변수들 간의 상관관계와 품위(MG) 및 회수율(MR)을 예측할 수 있는 모델식을 도출하였다. 억제제 농도+세척수 속도 및 입도 크기+억제제 농도+세척수 속도의 요인들은 유의수준(0.05)보다 작아 종속변수인 품위에 뚜렷한 영향을 주고 있으며 회수율 모형의 경우, 입도 크기와 세척수의 요인만이 종속변수인 회수율에 영향을 주었다.

• 자원리싸이클링
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• 제19권2호
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• pp.35-44
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• 2010

신흥개발국과 선진국의 해외자원 확보 경쟁이 심화되는 가운데 대부분의 광물자원을 수입하고 있는 우리나라는 안정적인 자원확보 및 외화지출을 줄이기 위해 국내에 부존되어 있는 몰리브덴광 등을 재개발하기 시작하였다. 본 연구에서는 현재 국내에서 유일하게 몰리브덴광을 생산하고 있는 (주)동원NMC의 최종정광(Mo 50.4%)을 대상으로 XRD 및 성분분석 결과 석영과 Grossular, Hedenbergite 등이 불순문로 존재하였으며, 입도분석 결과 60~140 mesh의 비교적 조립질 구간에 Mo 57% 이상의 고품위로 구성되어 있음을 확인하였다. 또한, (주)동원NMC의 최종정광(Mo 50.4%)의 고품위 가능성 및 실수율 향상 가능성을 확인하기 위해 실험을 실시하였다. 그 결과 마광시간 15분, 포수제 Kerosene 0.1 l/ton, 기포제 AF 65 7.2 l/ton, 세척수량 630 ml/min., air flow rate 1,197 ml/min.의 조건에서 Mo 58.6% ($MoS_2$ 97.83%)의 산물을 87.47%의 실수율로 얻을 수 있었다.

• 자원환경지질
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• 제25권3호
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• pp.283-296
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• 1992

The Keumryeong deposits is a low grade copper deposits in which copper minerals form disseminated grains and thin veinlets in felsic volcanics seem to be dacite. Alteration of the volcanics consists mainly pervasive propylitization and silicification. Potassic alteration characterized by biotite developed locally adjacent to southwestern contact of granodiorite body. Principal sulfide minerals in altered zone are mainly pyrite and lesser chalcopyrite. Chalcopyrite content in potassic zone is relatively higher than that of surrounding propylitized zone. Pyrite and chalcopyrite accompanies magnetite, molybdenite, sphalerite, pyrrhotite, arsenopyrite, pentlandite, marcasite, hematite, ilmenite, rutile, bismuthinite and native Bi as disseminations, veinlets and knots. Granodiorite body is propylitized and contains veinlets of pyrite, chalcopyrite and molybdenite. Fluid inclusions in sulfide-bearing quartz veinlets and quartz grains of felsic volcanics and granodiorite in altered zone consist of liquid-rich, vapor-rich, $CO_2-bearing$ and halite-bearing inclusions. These four types of inclusion intimately associated on a microscopic scale and indicate condensing or boiling of ore fluid during mineralization. Homogenization temperature of coexisting fluid inclusions are mostly in the range of 350 to $450^{\circ}C$. High salinity fluid contains 28.6 to 48.4 weight percent NaCI equivalent and moderate salinity fluid cotains 0.5 to 12.5 weight percent NaCl equivalent. Pressure estimated from $CO_2$ mole fraction of $CO_2-bearing$ inclusion range 160 to 375 bars. The Kigu copper deposits is a fissure filling copper vein developed 500 m south from the Keumryong deposits. Mineralogy and fluid inclusion data of the Kigu deposits are similar to that of the Keumryeong deposits. Homogenization temperature of fluid inclusions from the Kigu deposits are reasonable agreement with temperature estimated from sulfidation curve of cubanite-chalcopyrite-pyrite-pyrrhotite and pyrite-pyrrhotite mineral assemblages. Not only mineral occurrence and wall rock alteration in the Keumryeong deposits but also fluid inclusion data such as temperature, salinity, pressure and boiling evidences are similar to those of porphyry copper deposits.

• 한국정보컨버전스학회:학술대회논문집
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• 한국정보컨버전스학회 2008년도 International conference on information convergence
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• pp.99-102
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• 2008

Mineralogical studies of ore and alteration minerals have been conducted for the Hugo Dummett porphyry copper deposit. The Hugo Dummett porphyry copper gold deposit is located in the South Gobi region, Mongolia and currently being explored. This deposit divided into the Cu-rich Hugo Dummett South and the Cu-Au-rich Hugo Dummett North deposits. The Hugo Dummett deposits contain 1.08% copper(1.16 billion tonnes in total) and 0.23 g/t gold(Oyunchimeg et al., 2006). Copper-gold mineralization at these deposit are centered on a high-grade copper(typically>2.5%) and gold(0.5-2 g/t) zone of intense quartz stockwork veining. The high grade copper and gold zone is mainly within the Late Devonian quartz monzodiorite intrusions and augite basalt, also locally occurs in dacitic rocks. Intense quartz veining forms a lens up to 100 m wide hosted by augite basalt and partly by quartz monzodiorite. Although many explorations have been carried out, only a few scientific works were done in the Oyu Tolgoi mining area. Therefore the nature of copper-gold mineralization and orgin of the deposit is not fully understood. Copper-gold mineralization in the Hugo Dummett deposits occurs in dominantly quartz monzodiorite and minor augite basalt, dacitic rocks and locally biotite granodiorite. Chalcopyrite, pyrite, bornite, molybdenite, tennantite, tetrahedrite, enargite, sphalerite, chalcocite, covellite, eugenite, galena and gold occur as main ore minerals in the Hugo Dummett North and South deposits. These sulfides occur as: (1) a vague vein-like trail 1-3cm long and 2-3 mm wide, (2) minute, discontinuous cracks within quartz(micron scales), and (3) irregular blebs/spots(micron scales)and (4) disseminated within the sericite and plagioclase, commonly concentrated in the quartz. Sulfide minerals commonly display as a replacement, intergrown and minor exsolution texture in the both of the Hugo Dummet deposits.

• 자원환경지질
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• 제27권1호
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• pp.11-28
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• 1994

The Anyang Feldspar Mine is located in Seoksu Dong, Anyang City, Kyeonggi Do, Korea and has a long exploitation record that is once produced high grade sodium feldspars, for glaze. Geologically, This area is mainly composed of Mesozoic Jurassic biotite granite (Anyang granite) which intruded Precambrian Kyeonggi Gneiss Complex outcroped near the mining area. The deposit is localized on the southwest hill side of Anyang granite batholith and is confined in hydrothemal alteration zone formed by sodium-rich alkali hydrothermal fluids along the fractures of leucocratic granite showing later differentiation facies in the biotite granite. The hydrothermal alteration is characterized by albitization, sericitization, and desilication. The microscopic observation and EPMA, XRD analysis of the feldspar ores show that major minerals are albite and quartz and accessory minerals are orthoclase and sericite, and they are rarely associated with perthite, fluorite, zircon, kaolinite, molybdenite, microcline and iron-oxide. In the REE pattern, the strong negative Eu anomalies of the feldspar ores indicate the influence of feldspar fractionation and show similiar pattern of the host leucocratic granite. The filling temperature of quartz crystals in ore zone ranges from $276^{\circ}C$ to $342^{\circ}C$, and it is inferred that the alteration occurred by the hypothermal solution.