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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)

Paleomagnetic directional groups and paleointensity from the flood basalt in the Tarim large igneous province: Implications for eruption frequency 1. Geomagnetism

https://doi.org/10.24517/00067001
https://doi.org/10.24517/00067001
151f7057-db1d-4bd9-9cd6-327fd71d91dd
名前 / ファイル ライセンス アクション
TE-PR-USUI-Y-69-14.pdf SC-PR-USUI-Y-69-14.pdf (1.9 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 Paleomagnetic directional groups and paleointensity from the flood basalt in the Tarim large igneous province: Implications for eruption frequency 1. Geomagnetism
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 10.24517/00067001
ID登録タイプ JaLC
著者 Usui, Yoichi

× Usui, Yoichi

WEKO 106521
e-Rad 20609862

Usui, Yoichi

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Tian, Wei

× Tian, Wei

WEKO 106524

Tian, Wei

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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 Earth, Planets and Space

巻 69, 号 1, p. 14, 発行日 2017
ISSN
収録物識別子タイプ ISSN
収録物識別子 1880-5981
NCID
収録物識別子タイプ NCID
収録物識別子 AA11211921
DOI
関連タイプ isIdenticalTo
識別子タイプ DOI
関連識別子 10.1186/s40623-016-0595-x
出版者
出版者 Springer Berlin
抄録
内容記述タイプ Abstract
内容記述 We present paleomagnetic secular variation and paleointensity from the Early Permian Tarim large igneous province, NW China. The studied sections comprise a total of ~400 m of basaltic flows. Paleomagnetic directions were determined for 11 flows. Four successive flows with a cumulative thickness of ~150 m showed a statistically identical paleomagnetic direction. Assuming a paleosecular variation speed similar to that of the present day, the ~150-m-thick basalt was estimated to have erupted within the past few centuries. Paleointensity experiments were performed on both whole-rock and single plagioclase samples. Although alterations during the experiment and/or weak remanence degraded the data quality, the flows with the same paleomagnetic direction revealed similar paleointensity estimates, supporting the hypothesis that the eruption of these flows was rapid. More generally, flows from the Lower Kupukuziman Formation seem to record lower paleointensity compared to flows from the overlying Kaipaizileike Formation. [Figure not available: see fulltext. Caption: Left the extent of the Tarim large igneous province. Center in-situ paleomagnetic directions obtained from the Tarim large igneous province. Subashi and Yingan represents directions reported in a previous research. Right tilt-corrected paleomagnetic directions. Tight clustering of the direction indicate fast eruption relative to the paleomagnetic secular variation (PSV) speed. © 2017 The Author(s).
権利
権利情報 Copyright © The Author(s) 2017.
権利
権利情報 This article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
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://earth-planets-space.springeropen.com/articles/10.1186/s40623-016-0595-x
関連名称 https://earth-planets-space.springeropen.com/articles/10.1186/s40623-016-0595-x
関連URI
識別子タイプ URI
関連識別子 https://earth-planets-space.springeropen.com/
関連名称 https://earth-planets-space.springeropen.com/
関連URI
識別子タイプ URI
関連識別子 https://www.springeropen.com/
関連名称 https://www.springeropen.com/
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