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  1. 紀要
  2. 理工学部
  3. 国士舘大学 理工学部紀要
  4. 第11号(平成29年11月)

Estimated peak metamorphic temperature of the Sanbagawa schists from Nagatoro area, Kanto Mountains, using Raman microspectrometry on carbonaceous materials

https://kokushikan.repo.nii.ac.jp/records/13425
https://kokushikan.repo.nii.ac.jp/records/13425
bd0e7d03-b576-4731-b8be-b1f789c342d2
名前 / ファイル ライセンス アクション
1882_4013_011_09.pdf 本文 (1.8 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2018-11-01
タイトル
タイトル Estimated peak metamorphic temperature of the Sanbagawa schists from Nagatoro area, Kanto Mountains, using Raman microspectrometry on carbonaceous materials
言語 en
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 departmental bulletin paper
関連タイトル
値 理工学部発足10周年記念号
見出し
大見出し 論文
言語 ja
見出し
大見出し Original Paper
言語 en
著者 乾, 睦子

× 乾, 睦子

WEKO 25060
J-GLOBAL ID 200901080089470279
e-Rad_Researcher 10338296
AID DA17790666
国立国会図書館典拠データ 001142425
VIAF 305101591
ISNI 0000000418183394
ORCID 0000-0003-4850-207X

ja 乾, 睦子
ISNI

ja-Kana イヌイ, ムツコ

en Inui, Mutsuko


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Izumi, Rio

× Izumi, Rio

WEKO 20963

ja Izumi, Rio
ISNI


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Watanabe, Taiga

× Watanabe, Taiga

WEKO 20964

en Watanabe, Taiga

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著者ID
内容記述タイプ Other
内容記述 J-GLOBAL : 200901080089470279
著作関係者詳細
値 Izumi Rio : Kanagawa Prefectural Police
Watanabe Taiga : Chiba prefectural junior high school
抄録
内容記述タイプ Abstract
内容記述 The deformation regime of the Sanbagawa metamorphic rocks of the Kanto Mountains have long been controversial, whether it is one plastic continuous body or it is composed of several parts separated by faults or thrusts. One of the key must lie in the area where rocks with different mineral assemblage are found adjacent to each other. Most of the Nagatoro area is categorized as the lowest metamorphic grade zone which is defined by the mineral assemblage without garnet. Several outcrops in this area are known to contain garnet. It has been argued that the appearance of garnet indicates juxtaposition of rocks from different metamorphic grade, suggesting structural discontinuity. To investigate whether the local garnet occurrence was the discontinuity, Raman microspectrometry was applied carbonaceous materials in 27 rock samples in a continuous outcrop in this study. The estimated temperature was 400 to 460℃ with no structural gap or tendency recognizable when mapped. Samples with and without garnet both produced results comparable to each other. No evidence was obtained to show that the local garnet occurrence at the outcrop is due to structural discontinuity. The estimated temperature range was consistent with the beginning condition of the garnet formation. It is likely that the boundary between the garnet bearing rocks and those without garnet was originally continuous, with the condition just on the border to start growing garnet.
書誌情報 国士舘大学理工学部紀要
en : TRANSACTIONS OF THE KOKUSHIKAN UNIVERSITY SCHOOL OF SCIENCE AND ENGINEERING

巻 11, p. 55-60, 発行日 2017-11-30
出版者
出版者 国士舘大学理工学部
ISSN
収録物識別子タイプ PISSN
収録物識別子 1882-4013
NCID
収録物識別子タイプ NCID
収録物識別子 AA12316266
論文ID(NAID)
関連タイプ isIdenticalTo
識別子タイプ NAID
関連識別子 40021625215
NDC
主題Scheme NDC
主題 455.1
フォーマット
内容記述タイプ Other
内容記述 application/pdf
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
キーワード
主題 Garnet, Sanbagawa metamorphic belt, Kanto Mountains, temperature, Raman spectrometry
関東山地, 三波川変成帯
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