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  1. 防災科研関係論文

He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea

https://nied-repo.bosai.go.jp/records/4233
https://nied-repo.bosai.go.jp/records/4233
d109b1b7-6fd8-499b-856c-6fa2a9c83213
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル He-Ar-H-O isotopic signatures in Au-Ag bearing ore fluids of the Sunshin epithermal gold-silver ore deposits, South Korea
言語
言語 eng
著者 Kyu Han Kim

× Kyu Han Kim

en Kyu Han Kim

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Seungyeol Lee

× Seungyeol Lee

en Seungyeol Lee

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Keisuke Nagao

× Keisuke Nagao

en Keisuke Nagao

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Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

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Kyounghee Yang

× Kyounghee Yang

en Kyounghee Yang

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Jong Ik Lee

× Jong Ik Lee

en Jong Ik Lee

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内容記述タイプ Other
内容記述 Helium (He-3/He-4), argon (Ar-40/Ar-36) and oxygen (O-18/O-16) isotopic ratios in fluid inclusions trapped in quartz and pyrite from the Sunshin epithermal gold-silver ore deposits in South Korea were analyzed to investigate the magmatic contribution to ore forming fluids. Mantle helium with high He-3/He-4 ratios (up to He-3/He-4 similar to 9R(A), where R-A = 1.4 x 10(-6) for air) were identified from fluid inclusions in auriferous quartz veins, which are characterized as low sulfidation (adularia-sericite) type. The ratios provide direct evidence of links between low sulfidation ore fluids in epithermal gold deposits and magma from a mantle source. Interestingly, the oxygen and hydrogen isotopic compositions of the ore fluids (delta O-18= - 1.9 to - 6.6%., delta D = - 82 to - 100%.), calculated from ore quartz, indicate that meteoric waters were predominant during precipitation of the Au-Ag ore. Microthermometric measurements for fluid inclusions indicate relatively low temperatures (<= 300 degrees C) for the formation of the low sulfidation epithermal ore deposits. (C) 2012 Elsevier B.V. All rights reserved.
言語 en
書誌情報 en : CHEMICAL GEOLOGY

巻 320, p. 128-139
出版者
言語 en
出版者 ELSEVIER SCIENCE BV
ISSN
収録物識別子タイプ ISSN
収録物識別子 0009-2541
DOI
関連識別子 10.1016/j.chemgeo.2012.05.027
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