WEKO3
インデックスリンク
アイテム
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福井県勝山市九頭竜川上流地域の黒雲母斑晶に富む高カリウム玄武岩質転石
https://doi.org/10.24517/00063616
https://doi.org/10.24517/000636160fdb8080-3d4c-4cf7-b140-ddb4c6a1851b
名前 / ファイル | ライセンス | アクション |
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SC-PR-MORISHITA-T-941.pdf (5.0 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-08-30 | |||||
タイトル | ||||||
タイトル | 福井県勝山市九頭竜川上流地域の黒雲母斑晶に富む高カリウム玄武岩質転石 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Biotite phenocryst-rich high-K basaltic boulder from upper stream of the Kuzuryu River in Katsuyama City, Fukui Prefecture | |||||
言語 | ||||||
言語 | jpn | |||||
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 | 10.24517/00063616 | |||||
ID登録タイプ | JaLC | |||||
著者 |
森下, 知晃
× 森下, 知晃× 町, 澄秋× ファン, ミゲル グオターナ× 田村, 明弘 |
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著者別表示 |
Morishita, Tomoaki
× Morishita, Tomoaki× 町, 澄秋× Guotana, Juan Miguel× Tamura, Akihiro |
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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自然システム学系 | |||||
書誌情報 |
地質学雑誌 en : The Journal of the Geological Society of Japan 巻 124, 号 11, p. 941-946, 発行日 2018-11-15 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0016-7630 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1349-9963 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00141768 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.5575/geosoc.2018.0031 | |||||
出版者 | ||||||
出版者 | 日本地質学会 The Geological Society of Japan | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Boulders of biotite-phenocryst-rich, high-K basaltic rock were discovered in the upper stream of the Kuzuryu River in Katsuyama City, Fukui Prefecture. The biotite phenocrysts are zoned, with pale brown cores and dark brown margins. Relics of mafic minerals, replaced by carbonate minerals, contain chromian spinel. Although the primary chemical composition is affected by the formation of secondary minerals such as carbonate, the SiO2 and K2O contents of the studied rock are 48-49 wt% and 3.6 wt%, respectively, which are within the chemical range of absarokite. Chondrite-normalized rare earth element and primitive-mantle-normalized trace element patterns of the studied volcanic rocks are characterized by high LREEs/HREEs, high concentrations of LILEs, and negative anomalies of HFSEs (Nb, Ti). These petrological and geochemical characteristics represent a primary composition that has never before been reported in the Hokuriku district. | |||||
権利 | ||||||
権利情報 | Copyright © 日本地質学会 The Geological Society of Japan | |||||
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 | http://www.geosociety.jp | |||||
関連名称 | http://www.geosociety.jp | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/ | |||||
関連名称 | https://www.jstage.jst.go.jp/browse/geosoc/-char/ja/ |