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  1. 原著論文

U-Th radioactive disequilibrium and ESR dating of a barite-containing sulfide crust from South Mariana Trough

https://repo.qst.go.jp/records/47310
https://repo.qst.go.jp/records/47310
4025a678-0429-4207-b0be-76719ed1a8f9
Item type 学術雑誌論文 / Journal Article(1)
公開日 2015-09-28
タイトル
タイトル U-Th radioactive disequilibrium and ESR dating of a barite-containing sulfide crust from South Mariana Trough
言語
言語 eng
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 metadata only access
アクセス権URI http://purl.org/coar/access_right/c_14cb
著者 Takamasa, Asako

× Takamasa, Asako

WEKO 473248

Takamasa, Asako

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Nakai, Shun'ichi

× Nakai, Shun'ichi

WEKO 473249

Nakai, Shun'ichi

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Sato, Fumihiro

× Sato, Fumihiro

WEKO 473250

Sato, Fumihiro

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Toyoda, Shin

× Toyoda, Shin

WEKO 473251

Toyoda, Shin

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Debabrata, Banerjee

× Debabrata, Banerjee

WEKO 473252

Debabrata, Banerjee

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賞雅 朝子

× 賞雅 朝子

WEKO 473253

en 賞雅 朝子

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抄録
内容記述タイプ Abstract
内容記述 A block of sulfide crust collected from an active hydrothermal mound in an Archaean site (12°56.4′N, 143°37.9′E; depth ca. 3000 m) of the South Mariana Trough was dated using both 230Th/234U disequilibrium and electron spin resonance (ESR) methods to establish the growth duration. Eight subsamples from the sulfide crust were separated further into magnetic and non-magnetic fractions using a Franz isodynamic separator. Thirteen sulfide samples, soluble in nitric acid, yielded 230Th/234U ages of 0.3–2.2 ka. The magnetic fractions had significantly lower Th/U ratios, which enabled age determinations as precise as ±2% (2σ). The age distribution obtained for the section of sulfide crust analyzed is consistent with deposition of sulfide minerals from the upper surface of the crust to the inner side. The 230Th/234U ages of the sulfide minerals were compared with ESR ages of barites separated from 12 subsamples of the same sulfide crust. ESR ages of 0.27–1.3 ka show a spatial pattern broadly resembling that observed in 230Th/234U dating method. While there are some significant offsets, these results illustrate the potential of the two methods for use in investigation of the evolutional history of a hydrothermal system.
書誌情報 Quaternary Geochronology

巻 15, p. 38-46, 発行日 2012-12
ISSN
収録物識別子タイプ ISSN
収録物識別子 1871-1014
関連サイト
識別子タイプ URI
関連識別子 http://www.sciencedirect.com/science/article/pii/S1871101412001896
関連名称 http://www.sciencedirect.com/science/article/pii/S1871101412001896
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