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Large Amount of Excess Argon in Hydrothermal Quartz from the Vangtat Orogenic Gold Belt, Southern Laos: New In-Sight from K-Ar and Noble Gas Isotope Analyses
http://hdl.handle.net/10295/00006262
http://hdl.handle.net/10295/00006262100d86b2-c7b4-4e22-96a0-8146de078034
名前 / ファイル | ライセンス | アクション |
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chihoA_2022_1.pdf (3.0 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||||||||
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公開日 | 2023-02-23 | |||||||||||
タイトル | ||||||||||||
タイトル | Large Amount of Excess Argon in Hydrothermal Quartz from the Vangtat Orogenic Gold Belt, Southern Laos: New In-Sight from K-Ar and Noble Gas Isotope Analyses | |||||||||||
言語 | en | |||||||||||
言語 | ||||||||||||
言語 | eng | |||||||||||
主題 | ||||||||||||
主題Scheme | Other | |||||||||||
主題 | noble gas isotopes | |||||||||||
主題 | ||||||||||||
主題Scheme | Other | |||||||||||
主題 | in vacuo crushing method | |||||||||||
主題 | ||||||||||||
主題Scheme | Other | |||||||||||
主題 | hydrothermal quartz | |||||||||||
主題 | ||||||||||||
主題Scheme | Other | |||||||||||
主題 | Thongkai-Ok | |||||||||||
主題 | ||||||||||||
主題Scheme | Other | |||||||||||
主題 | Vangtat | |||||||||||
主題 | ||||||||||||
主題Scheme | Other | |||||||||||
主題 | excess argon | |||||||||||
資源タイプ | ||||||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||||||
資源タイプ | journal article | |||||||||||
アクセス権 | ||||||||||||
アクセス権 | open access | |||||||||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||||||||
作成者 |
Bounliyong, Patthana
× Bounliyong, Patthana
× Sumino, Hirochika
× Arribas, Antonio
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内容記述 | ||||||||||||
内容記述タイプ | Abstract | |||||||||||
内容記述 | K-Ar dating and He-3/He-4 and Ar-40/Ar-36 analyses were conducted on samples of hydrothermal quartz from the Thongkai-Ok Au deposit in the Vangtat orogenic Au belt of southern Laos to study the presence of excess argon in hydrothermal quartz and to better understand the origin of the ore-forming fluids. The K-Ar age of two hydrothermal quartz separates yielded apparent dates of 1040 and 1385 Ma. These ages are significantly older than the estimated age of Vangtat Au mineralization (similar to 200 Ma) and other regional geologic events, indicating the presence of an extraordinary amount of excess argon in the hydrothermal quartz crystals. In vacuo crushing analyses of the Thongkai-Ok hydrothermal vein quartz delivered He-3/He-4 approximate to 0.2-0.3 R/Ra and Ar-40/Ar-36 approximate to 455-725, suggesting the ore-forming fluid is mainly derived from a crustal component with a minor contribution of mantle and meteoric fluids. | |||||||||||
言語 | en | |||||||||||
出版タイプ | ||||||||||||
出版タイプ | VoR | |||||||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||||||
書誌情報 |
en : MINERALS 巻 12, 号 10, 発行日 2022 |
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収録物識別子 | ||||||||||||
収録物識別子タイプ | ISSN | |||||||||||
収録物識別子 | 2075-163X | |||||||||||
出版者 | ||||||||||||
出版者 | MDPI | |||||||||||
言語 | en | |||||||||||
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関連タイプ | isIdenticalTo | |||||||||||
識別子タイプ | DOI | |||||||||||
関連識別子 | https://doi.org/10.3390/min12101205 | |||||||||||
権利情報 | ||||||||||||
権利情報 | © 2022 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/). |