광물과 암석 (Korean Journal of Mineralogy and Petrology)

  • 제33권3호
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  • Pages.195-214
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  • 2020
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  • 2734-0333(pISSN)
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  • 2734-0538(eISSN)
한국암석학회 & 한국광물학회 (The Petrological Society of Korea & The Mineralogical Society of Korea)
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삼광 금-은 광상에서 산출되는 함 티타늄 광물들의 산상 및 화학조성

Occurrence and Chemical Composition of Ti-bearing Minerals from Samgwang Au-ag Deposit, Republic of Korea

  • 유봉철 (한국지질자원연구원 DMR융합연구단)
  • Yoo, Bong Chul (Convergence Research Center for Development of Mineral Resources, Korea Institute of Geoscience and Mineral Resources)
  • 투고 : 2020.07.21
  • 심사 : 2020.09.03
  • 발행 : 2020.09.30
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초록

삼광 금-은 광상은 과거 한국에서 가장 큰 금-은 광상들 중의 하나였다. 이 광상은 선캠브리아기의 변성퇴적암류내에 발달된 열극대를 충진한 8개조의 석영맥으로 구성된 조산형 금-은 광상이다. 이 광상에서 함 티타늄 광물로는 설석, 티탄철석 및 금홍석이며 설석과 티탄철석은 모암에서만 산출되나 금홍석은 모암과 엽리상 석영맥에서 산출된다. 이들 광물들은 모암에선 흑운모, 백운모, 녹니석, 백색운모, 모나자이트, 저어콘 및 인회석과 엽리상 석영맥에선 백색운모, 녹니석 및 유비철석 등과 함께 산출된다. 설석은 최대 3.94 wt.% (Al2O3), 0.49 wt.% (FeO), 0.52 wt.% (Nb2O5), 0.46 wt.% (Y2O3) 및 0.43 wt.% (V2O5) 값을 갖는다. 이 설석은 0.06~0.14 (Fe/Al 비) 값으로 변성기원의 설석이고 XAl (=Al/Al+Fe3++Ti) 값이 0.06~0.15 값으로 저 함량 알루미늄 설석에 해당된다. 티탄철석은 최대 0.07 wt.% (ZrO2), 0.12 wt.% (HfO2), 0.26 wt.% (Nb2O5), 0.04 wt.% (Sb2O5), 0.13 wt.% (Ta2O5), 2.62 wt.% (As2O5), 0.29 wt.% (V2O5), 0.12 wt.% (Al2O3), 1.59 wt.% (ZnO)로써 As2O5 함량이 높게 산출된다. 금홍석의 화학조성은 모암과 엽리상 석영맥에서 각각 최대 0.35 wt.%, 0.65 wt.% (HfO2), 2.52 wt.%, 0.19 wt.% (WO3), 1.28 wt.%, 1.71 wt.% (Nb2O3), 0.03 wt.%, 0.07 wt.% (Sb2O3), 0.28 wt.%, 0.21 wt.% (As2O5), 0.68 wt.%, 0.70 wt.% (V2O3), 0.48 wt.%, 0.59 wt.% (Cr2O3), 0.70 wt.%, 1.90 wt.% (Al2O3), 4.76 wt.%, 3.17 wt.% (FeO)로써 엽리상 석영맥의 금홍석에서 HfO2, Nb2O3, As2O5, Cr2O3, Al2O3 및 FeO 원소들의 함량이 모암의 금홍석보다 높지만 WO3 원소의 함량은 낮다. 이 미량원소들은 모암의 금홍석[(Fe3+, Al3+, Cr3+) + Hf4++(W5+, As5+, Nb5+) ⟵⟶; 2Ti4++ V4+, 2Fe2++(Al3+, Cr3+) + Hf4++(W5+, As5+, Nb5+) ⟵⟶ 2Ti4++2V4+], 엽리상 석영맥의 금홍석 [(Fe3+, Al3+) + As5+ ⟵⟶ Ti4++ V4+, (Fe3+, Al3+) + As5+ ⟵⟶ Ti4++Hf4+, 4(Fe3+, Al3+) ⟵⟶ Ti4++(W5+, Nb5+) + Cr3+]로써 치환관계가 있었다. 이들 자료를 근거로, 모암내 산출되는 설석, 티탄철석 및 금홍석은 광역변성작용 동안 모암광물들의 변질 시 광물내 존재했던 W5+, Nb5+, As5+, Hf4+, V4+, Cr3+, Al3+, Fe3+, Fe2+ 등과 같은 양이온들의 재 용해 및 농집에 의해 형성되었다. 그후 계속된 연성전단 시 엽리상 석영맥내 금홍석은 열수 용액의 유입에 따른 백색운모와 녹니석의 모암변질작용에 의한 양이온들의 재 용해 및 재 농집과 더불어 초기에 형성된 설석, 티탄철석 및 금홍석과의 반응에 의해 기존에 이들 광물내에 존재하였던 Nb5+, As5+, Hf4+, Cr3+, Al3+, Fe3+, Fe2+과 같은 양이온들의 재농집에 의해 형성된 것으로 생각된다.

The Samgwang Au-Ag deposit has been one of the largest deposits in Korea. The deposit consists of eight lens-shaped quartz veins which filled fractures along fault zones in Precambrian metasedimentary rock, which feature suggest that it is an orogenic-type deposit. The Ti-bearing minerals occur in wallrock (titanite, ilmenite and rutile) and laminated quartz vein (rutile). They occur minerals including biotite, muscovite, chlorite, white mica, monazite, zircon, apatite in wallrock and white mica, chlorite, arsenopyrite in laminated quartz vein. Chemical composition of titanite has maximum vaules of 3.94 wt.% (Al2O3), 0.49 wt.% (FeO), 0.52 wt.% (Nb2O5), 0.46 wt.% (Y2O3) and 0.43 wt.% (V2O5). Titanite with 0.06~0.14 (Fe/Al ratio) and 0.06~0.15 (XAl (=Al/Al+Fe3++Ti)) corresponds with metamorphic origin and low-Al variety. Chemical composition of ilmenite has maximum values of 0.07 wt.% (ZrO2), 0.12 wt.% (HfO2), 0.26 wt.% (Nb2O5), 0.04 wt.% (Sb2O5), 0.13 wt.% (Ta2O5), 2.62 wt.% (As2O5), 0.29 wt.% (V2O5), 0.12 wt.% (Al2O3) and 1.59 wt.% (ZnO). Chemical composition of rutile in wallrock and laminated quartz vein has maximum values of 0.35 wt.%, 0.65 wt.% (HfO2), 2.52 wt.%, 0.19 wt.% (WO3), 1.28 wt.%, 1.71 wt.% (Nb2O3), 0.03 wt.%, 0.07 wt.% (Sb2O3), 0.28 wt.%, 0.21 wt.% (As2O5), 0.68 wt.%, 0.70 wt.% (V2O3), 0.48 wt.%, 0.59 wt.% (Cr2O3), 0.70 wt.%, 1.90 wt.% (Al2O3) and 4.76 wt.%, 3.17 wt.% (FeO), respectively. Rutile in laminated quartz vein is higher contents (HfO2, Nb2O3, As2O5, Cr2O3, Al2O3 and FeO) and lower content (WO3) than rutile in wallrock. The substitutions of rutile in wallrock and laminated quatz vein are as followed : rutile in wallrock [(Fe3+, Al3+, Cr3+) + Hf4+ + (W5+, As5+, Nb5+) ⟵⟶ 2Ti4+ + V4+, 2Fe2+ + (Al3+, Cr3+) + Hf4+ + (W5+, As5+, Nb5+) ⟵⟶ 2Ti4+ + 2V4+], rutile in laminated quartz vein [(Fe3+, Al3+) + As5+ ⟵⟶ Ti4+ + V4+, (Fe3+, Al3+) + As5+ ⟵⟶ Ti4+ + Hf4+, 4(Fe3+, Al3+) ⟵⟶ Ti4+ + (W5+, Nb5+) + Cr3+], respectively. Based on these data, titanite, ilmenite and rutile in wallrock were formed by resolution and reconcentration of cations (W5+, Nb5+, As5+, Hf4+, V4+, Cr3+, Al3+, Fe3+, Fe2+) in minerals of wallrock during regional metamorphism. And then rutile in laminated quartz vein was formed by reconcentration of cations (Nb5+, As5+, Hf4+, Cr3+, Al3+, Fe3+, Fe2+) in alteration minerals (white mica, chlorite) and Ti-bearing minerals reaction between hydrothermal fluid originated during ductile shear and Ti-bearing minerals (titanite, ilmenite and rutile) in wallrock.

키워드

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