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  1. B. 理工学域; 数物科学類・物質化学類・機械工学類・フロンティア工学類・電子情報通信学類・地球社会基盤学類・生命理工学類
  2. b 10. 学術雑誌掲載論文
  3. 1.査読済論文(理)

Evidence for a 3.45-billion-year-old magnetic remanence: Hints of an ancient geodynamo from conglomerates of South Africa

https://doi.org/10.24517/00067005
https://doi.org/10.24517/00067005
eb9ec653-10a7-4e61-bcb5-7c7cfd97af20
名前 / ファイル ライセンス アクション
TE-PR-USUI-Y-10-Q09Z07.pdf SC-PR-USUI-Y-10-Q09Z07.pdf (1.3 MB)
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Item type 学術雑誌論文 / Journal Article(1)
公開日 2022-09-01
タイトル
タイトル Evidence for a 3.45-billion-year-old magnetic remanence: Hints of an ancient geodynamo from conglomerates of South Africa
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
ID登録
ID登録 10.24517/00067005
ID登録タイプ JaLC
著者 Usui, Yoichi

× Usui, Yoichi

WEKO 106521
e-Rad 20609862

Usui, Yoichi

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Tarduno, John A.

× Tarduno, John A.

WEKO 106533

Tarduno, John A.

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Watkeys, Michael

× Watkeys, Michael

WEKO 106534

Watkeys, Michael

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Hofmann, Axel

× Hofmann, Axel

WEKO 106535

Hofmann, Axel

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Cottrell, Rory D.

× Cottrell, Rory D.

WEKO 106536

Cottrell, Rory D.

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著者別表示 臼井, 洋一

× 臼井, 洋一

臼井, 洋一

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提供者所属
内容記述タイプ Other
内容記述 金沢大学理工研究域地球社会基盤学系
書誌情報 Geochemistry, Geophysics, Geosystems

巻 10, 号 9, p. Q09Z07, 発行日 2009-09-24
ISSN
収録物識別子タイプ ISSN
収録物識別子 1525-2027
DOI
関連タイプ isIdenticalTo
識別子タイプ DOI
関連識別子 10.1029/2009GC002496
出版者
出版者 American Geophysical Union, Geochemical Society / Wiley Open Access
抄録
内容記述タイプ Abstract
内容記述 Paleomagnetic and rock magnetic analyses of ̃3445-million-year-old dacite conglomerate clasts and parent body rocks from the Barberton greenstone belt, South Africa, define two dominant components of magnetization. One component, unblocked at low temperature, is an overprint acquired ̃180 million years ago. The other component is unblocked at high temperatures and passes a conglomerate test, indicating that this component is older than the depositional age of the conglomerate (̃3416 Ma). The high unblocking temperature component shows scatter in the parent body rocks that can be explained by the effects of modern lightning strikes, Archean overprinting, and the presence of multidomain magnetic grains that are conducive to carrying secondary magnetizations. Alternatively, this scatter can be explained by exotic magnetization scenarios in the absence of a dynamo, including magnetization by an external field related to solar wind interaction with the atmosphere. Such exotic mechanisms can be tested with the acquisition of paleointensity data. While more scattered than paleomagnetic data recording the more recent geomagnetic field, the high unblocking temperature component in the dacite parent body shows some consistency, and the simplest explanation of the data is that they reflect a geodynamõ3445 million years ago. © 2009 by the American Geophysical Union.
権利
権利情報 Copyright © 2009. American Geophysical Union.
著者版フラグ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
関連URI
識別子タイプ URI
関連識別子 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2009GC002496
関連名称 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2009GC002496
関連URI
識別子タイプ URI
関連識別子 https://agupubs.onlinelibrary.wiley.com/journal/15252027
関連名称 https://agupubs.onlinelibrary.wiley.com/journal/15252027
関連URI
識別子タイプ URI
関連識別子 http://sites.agu.org/
関連名称 http://sites.agu.org/
関連URI
識別子タイプ URI
関連識別子 https://authorservices.wiley.com/open-research/open-access/index.html
関連名称 https://authorservices.wiley.com/open-research/open-access/index.html
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