Origin of a dolomite-related jade deposit at Chuncheon, Korea

Tzen Fu Yui, Sung Tack Kwon

Research output: Contribution to journalArticle

28 Citations (Scopus)

Abstract

The Chuncheon nephrite deposit in Korea is among the largest nephrite jade deposits worldwide. The deposit is hosted in Precambrian dolomitic marble and amphibole schist that were intruded by the posttectonic (Late Triassic) Chuncheon granite. Carbonates in the dolomitic marble and nephrite deposit have oxygen and carbon isotope compositions in the range of -0.1 to + 18.2 per mil and -4.3 to + 0.9 per mil, and -0.4 to + 3.5 per mil and -9.9 to -4.7 per mil, respectively. These data are in agreement with decarbonation processes driven by fluid infiltration forming the nephrite deposit from dolomitic marble in the temperature range of 330° to 430°C. Stable isotope compositions of silicates from the nephrite deposit are homogeneous and extremely depleted in 18O and D; tremolite has δ 18O = -9.9 to -7.9 per mil and δD = 118 to -105 per mil; diopside has δ 18O = -13.6 to -11.5 per mil; three samples of grossular have δ 18O = -4.4, +10.4, and + 11.5 per mil; clinochlore has δ 18O = -9.5 to -9.0 per mil, and δD = -103 to -94 per mil; and two tale veins have δ 18O = -7.7 and -7.3 per mil, and δD = -86 and -90 per mil, Quartz and amphibole in nearby amphibole schists also have variable oxygen isotope compositions of -4.7 to +0.5 per mil and -8.4 to -0.6 per mil, respectively, and are not in isotopic equilibrium. It is suggested that the formation of this nephrite deposit postdated the metamorphism of the country rocks. The distinctly negative δ 18O values also indicate that the infiltrated fluid was mainly of meteoric origin and its circulation was most likely related to the intrusion of the nearby posttectonic Chuncheon granite. Model calculations demonstrate that the fluid/rock ratios were high, that both oxygen and hydrogen isotope compositions of nephrite were mainly buffered by the fluid phase, and that X cO2 of the fluid phase was very low during the nephrite formation. These conditions contrast with the formation of nephrite deposits that are spatially associated with serpentinites (e.g., Fengtien nephrite deposit, Taiwan). Such deposits are formed by fluid infiltration during regional metamorphism and their oxygen isotope compositions are mainly buffered by the host sepentinite.

Original languageEnglish
Pages (from-to)593-601
Number of pages9
JournalEconomic Geology
Volume97
Issue number3
DOIs
Publication statusPublished - 2002 May 1

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Korea
dolomite
Deposits
deposits
oxygen isotope
fluid
marble
Oxygen Isotopes
amphibole
Amphibole Asbestos
oxygen isotopes
Fluids
Calcium Carbonate
amphiboles
fluids
schist
infiltration
granite
Chemical analysis
clinochlore

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geology
  • Geochemistry and Petrology
  • Economic Geology

Cite this

@article{9318dbb2271547be83570495c24ffefa,
title = "Origin of a dolomite-related jade deposit at Chuncheon, Korea",
abstract = "The Chuncheon nephrite deposit in Korea is among the largest nephrite jade deposits worldwide. The deposit is hosted in Precambrian dolomitic marble and amphibole schist that were intruded by the posttectonic (Late Triassic) Chuncheon granite. Carbonates in the dolomitic marble and nephrite deposit have oxygen and carbon isotope compositions in the range of -0.1 to + 18.2 per mil and -4.3 to + 0.9 per mil, and -0.4 to + 3.5 per mil and -9.9 to -4.7 per mil, respectively. These data are in agreement with decarbonation processes driven by fluid infiltration forming the nephrite deposit from dolomitic marble in the temperature range of 330° to 430°C. Stable isotope compositions of silicates from the nephrite deposit are homogeneous and extremely depleted in 18O and D; tremolite has δ 18O = -9.9 to -7.9 per mil and δD = 118 to -105 per mil; diopside has δ 18O = -13.6 to -11.5 per mil; three samples of grossular have δ 18O = -4.4, +10.4, and + 11.5 per mil; clinochlore has δ 18O = -9.5 to -9.0 per mil, and δD = -103 to -94 per mil; and two tale veins have δ 18O = -7.7 and -7.3 per mil, and δD = -86 and -90 per mil, Quartz and amphibole in nearby amphibole schists also have variable oxygen isotope compositions of -4.7 to +0.5 per mil and -8.4 to -0.6 per mil, respectively, and are not in isotopic equilibrium. It is suggested that the formation of this nephrite deposit postdated the metamorphism of the country rocks. The distinctly negative δ 18O values also indicate that the infiltrated fluid was mainly of meteoric origin and its circulation was most likely related to the intrusion of the nearby posttectonic Chuncheon granite. Model calculations demonstrate that the fluid/rock ratios were high, that both oxygen and hydrogen isotope compositions of nephrite were mainly buffered by the fluid phase, and that X cO2 of the fluid phase was very low during the nephrite formation. These conditions contrast with the formation of nephrite deposits that are spatially associated with serpentinites (e.g., Fengtien nephrite deposit, Taiwan). Such deposits are formed by fluid infiltration during regional metamorphism and their oxygen isotope compositions are mainly buffered by the host sepentinite.",
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Origin of a dolomite-related jade deposit at Chuncheon, Korea. / Yui, Tzen Fu; Kwon, Sung Tack.

In: Economic Geology, Vol. 97, No. 3, 01.05.2002, p. 593-601.

Research output: Contribution to journalArticle

TY - JOUR

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N2 - The Chuncheon nephrite deposit in Korea is among the largest nephrite jade deposits worldwide. The deposit is hosted in Precambrian dolomitic marble and amphibole schist that were intruded by the posttectonic (Late Triassic) Chuncheon granite. Carbonates in the dolomitic marble and nephrite deposit have oxygen and carbon isotope compositions in the range of -0.1 to + 18.2 per mil and -4.3 to + 0.9 per mil, and -0.4 to + 3.5 per mil and -9.9 to -4.7 per mil, respectively. These data are in agreement with decarbonation processes driven by fluid infiltration forming the nephrite deposit from dolomitic marble in the temperature range of 330° to 430°C. Stable isotope compositions of silicates from the nephrite deposit are homogeneous and extremely depleted in 18O and D; tremolite has δ 18O = -9.9 to -7.9 per mil and δD = 118 to -105 per mil; diopside has δ 18O = -13.6 to -11.5 per mil; three samples of grossular have δ 18O = -4.4, +10.4, and + 11.5 per mil; clinochlore has δ 18O = -9.5 to -9.0 per mil, and δD = -103 to -94 per mil; and two tale veins have δ 18O = -7.7 and -7.3 per mil, and δD = -86 and -90 per mil, Quartz and amphibole in nearby amphibole schists also have variable oxygen isotope compositions of -4.7 to +0.5 per mil and -8.4 to -0.6 per mil, respectively, and are not in isotopic equilibrium. It is suggested that the formation of this nephrite deposit postdated the metamorphism of the country rocks. The distinctly negative δ 18O values also indicate that the infiltrated fluid was mainly of meteoric origin and its circulation was most likely related to the intrusion of the nearby posttectonic Chuncheon granite. Model calculations demonstrate that the fluid/rock ratios were high, that both oxygen and hydrogen isotope compositions of nephrite were mainly buffered by the fluid phase, and that X cO2 of the fluid phase was very low during the nephrite formation. These conditions contrast with the formation of nephrite deposits that are spatially associated with serpentinites (e.g., Fengtien nephrite deposit, Taiwan). Such deposits are formed by fluid infiltration during regional metamorphism and their oxygen isotope compositions are mainly buffered by the host sepentinite.

AB - The Chuncheon nephrite deposit in Korea is among the largest nephrite jade deposits worldwide. The deposit is hosted in Precambrian dolomitic marble and amphibole schist that were intruded by the posttectonic (Late Triassic) Chuncheon granite. Carbonates in the dolomitic marble and nephrite deposit have oxygen and carbon isotope compositions in the range of -0.1 to + 18.2 per mil and -4.3 to + 0.9 per mil, and -0.4 to + 3.5 per mil and -9.9 to -4.7 per mil, respectively. These data are in agreement with decarbonation processes driven by fluid infiltration forming the nephrite deposit from dolomitic marble in the temperature range of 330° to 430°C. Stable isotope compositions of silicates from the nephrite deposit are homogeneous and extremely depleted in 18O and D; tremolite has δ 18O = -9.9 to -7.9 per mil and δD = 118 to -105 per mil; diopside has δ 18O = -13.6 to -11.5 per mil; three samples of grossular have δ 18O = -4.4, +10.4, and + 11.5 per mil; clinochlore has δ 18O = -9.5 to -9.0 per mil, and δD = -103 to -94 per mil; and two tale veins have δ 18O = -7.7 and -7.3 per mil, and δD = -86 and -90 per mil, Quartz and amphibole in nearby amphibole schists also have variable oxygen isotope compositions of -4.7 to +0.5 per mil and -8.4 to -0.6 per mil, respectively, and are not in isotopic equilibrium. It is suggested that the formation of this nephrite deposit postdated the metamorphism of the country rocks. The distinctly negative δ 18O values also indicate that the infiltrated fluid was mainly of meteoric origin and its circulation was most likely related to the intrusion of the nearby posttectonic Chuncheon granite. Model calculations demonstrate that the fluid/rock ratios were high, that both oxygen and hydrogen isotope compositions of nephrite were mainly buffered by the fluid phase, and that X cO2 of the fluid phase was very low during the nephrite formation. These conditions contrast with the formation of nephrite deposits that are spatially associated with serpentinites (e.g., Fengtien nephrite deposit, Taiwan). Such deposits are formed by fluid infiltration during regional metamorphism and their oxygen isotope compositions are mainly buffered by the host sepentinite.

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