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  1. 学会発表・講演等
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ESR, 226Ra-210Pb and 228Ra-228Th Dating of Barite in Sea-Floor Hydrothermal Sulfide Deposits in the Okinawa Trough

https://repo.qst.go.jp/records/71605
https://repo.qst.go.jp/records/71605
8ea16843-3d81-45c3-b66d-7578d659f98c
Item type 会議発表用資料 / Presentation(1)
公開日 2015-04-20
タイトル
タイトル ESR, 226Ra-210Pb and 228Ra-228Th Dating of Barite in Sea-Floor Hydrothermal Sulfide Deposits in the Okinawa 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_c94f
資源タイプ conference object
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 Fujiwara, Taisei

× Fujiwara, Taisei

WEKO 704263

Fujiwara, Taisei

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Toyoda, Shin

× Toyoda, Shin

WEKO 704264

Toyoda, Shin

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Uchida, Ai

× Uchida, Ai

WEKO 704265

Uchida, Ai

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Ishibashi, Jun-Ichiro

× Ishibashi, Jun-Ichiro

WEKO 704266

Ishibashi, Jun-Ichiro

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Nakai, Shun'ichi

× Nakai, Shun'ichi

WEKO 704267

Nakai, Shun'ichi

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Takamasa, Asako

× Takamasa, Asako

WEKO 704268

Takamasa, Asako

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賞雅 朝子

× 賞雅 朝子

WEKO 704269

en 賞雅 朝子

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抄録
内容記述タイプ Abstract
内容記述 ESR (electron spin resonance) dating method has been
applied to calcite, aragonite, hydroxyapatite, quartz and
gypsum. Recently it was shown that this method is also
practically applicable to barite, especially those in sea-floor
hydrothermal sulfide deposits (Takamasa et al., 2013).
ESR, 226Ra-
210Pb, and 228Ra-
228Th ages were determined for
barite crystals extracted from hydrothermal sulfide deposits
taken at hydrothermal fields at the Okinawa Trough. The ages
range 4.1 to 16000 years where the ages obtained by the three
methods coincide in some of the samples while the 228Ra-
228Th
ages are the youngest and ESR ages, the oldest and the 226Ra- 210Pb ages in between in the other samples. The samples with
younger ESR ages show younger 226Ra-
210Pb ages and those
with older ESR ages show older 226Ra-
210Pb ages with no
detection of 228Ra. The inconsistency of the ages between these
methods would be explained by the mixture of the barite
crystals with younger and older ages, formed by several
hydrothermal activities. The order of ages of the 5
hydrothermal fields would be arranged, from young to old as
follows; Yoron Hole field, Daiyon-Yonaguni Knoll field,
Hatoma Knoll field, being nearly equal to Iheya North Knoll
field.
会議概要(会議名, 開催地, 会期, 主催者等)
内容記述タイプ Other
内容記述 Goldschmidt2014
発表年月日
日付 2014-06-12
日付タイプ Issued
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