ログイン
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

  1. 学術雑誌論文等

Investigation of the records of earthquake slip in carbonaceous materials from the Taiwan Chelungpu fault by means of infrared and Raman spectroscopies

https://hiroshima.repo.nii.ac.jp/records/2006925
https://hiroshima.repo.nii.ac.jp/records/2006925
556af1be-f2b2-4065-a62a-a6e0e7eabf62
名前 / ファイル ライセンス アクション
GeochemGeophyGeosys_16_1233.pdf GeochemGeophyGeosys_16_1233.pdf (3.1 MB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Investigation of the records of earthquake slip in carbonaceous materials from the Taiwan Chelungpu fault by means of infrared and Raman spectroscopies
言語 en
作成者 Hirono, Tetsuro

× Hirono, Tetsuro

en Hirono, Tetsuro

Search repository
Maekawa, Yuka

× Maekawa, Yuka

en Maekawa, Yuka

Search repository
Yabuta, Hikaru

× Yabuta, Hikaru

en Yabuta, Hikaru

Search repository
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
権利情報
権利情報 An edited version of this paper was published by AGU. Copyright 2015 American Geophysical Union.
主題
主題Scheme Other
主題 carbonaceous material
主題
主題Scheme Other
主題 Chelungpu fault
主題
主題Scheme Other
主題 1999 Chi‐Chi earthquake
主題
主題Scheme Other
主題 frictional heat
主題
主題Scheme Other
主題 fault gouge
内容記述
内容記述 To understand the mechanism of fault lubrication during the 1999 Taiwan Chi‐Chi earthquake, we developed a new temperature proxy for carbonaceous materials by using infrared and Raman spectroscopies together with heating and friction experiments. We found marked anomalies in the infrared and Raman spectra of carbonaceous materials retrieved from the primary slip zone of the earthquake: the infrared spectra exhibited very weak aliphatic CH2 and CH3 peaks and aromatic C=C absorbance peaks, and the Raman spectra exhibited very weak disordered and graphitic bands and a high ratio of disordered band area to graphitic band area. Those weak peaks and bands and the band area ratio were reproduced by heating carbonaceous materials from the nearby host rock to 700°C. These results suggest that the frictional heat in the slip zone reached approximately 700°C. We characterized the host rock's carbonaceous materials by means of elemental analysis, pyrolysis‐gas chromatography‐mass spectrometry, and simultaneous thermogravimetry‐differential scanning calorimetry and found that the H/C and O/C ratios were 1.29 and 0.30, respectively (which are close to the ratios for lignin) and that the volatile fraction was as high as 48 wt %. The pyrolysates obtained by heating from 100 to 400°C were dominated by phenols, fatty alcohols, and n‐alkanes. When the residue from pyrolysis at 100–400°C was rapidly heated to 700°C, the resulting pyrolysate was dominated by phenols, aromatic compounds, heterocyclic compounds, and n‐alkenes. This information suggests that change in the infrared and Raman spectra with increasing temperature may have been due to decomposition and aromatization reactions during pyrolysis. Rapid heating during earthquake slip may promote reactions of carbonaceous materials that are different from the reactions that occur during long‐term geological metamorphism.
言語 en
内容記述
内容記述タイプ Other
内容記述 This research was supported by a Grant-in-Aid for Young Scientists (A) from the Japan Ministry of Education, Science, Sports, and Culture (23684039, 2013).
出版者
出版者 American Geophysical Union
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
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
関連情報
識別子タイプ DOI
関連識別子 10.1002/2014GC005622
関連情報
識別子タイプ DOI
関連識別子 https://doi.org/10.1002/2014GC005622
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 1525-2027
開始ページ
開始ページ 1233
書誌情報 Geochemistry, Geophysics, Geosystems
Geochemistry, Geophysics, Geosystems

巻 16, 号 5, p. 1233-1253, 発行日 2015-05-02
旧ID 48719
戻る
0
views
See details
Views

Versions

Ver.1 2025-02-21 03:36:05.468494
Show All versions

Share

Mendeley Twitter Facebook Print Addthis

Cite as

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR 2.0
  • OAI-PMH JPCOAR 1.0
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3


Powered by WEKO3