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Thick and anisotropic D″ layer beneath Antarctic Ocean
https://doi.org/10.24517/00010168
https://doi.org/10.24517/00010168ad4960a1-1ae5-4552-8e5e-3b1b5fc2f2ff
名前 / ファイル | ライセンス | アクション |
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SC-PR-USUI-Y-321314.pdf (189.7 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2017-10-03 | |||||
タイトル | ||||||
タイトル | Thick and anisotropic D″ layer beneath Antarctic Ocean | |||||
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 | 10.24517/00010168 | |||||
ID登録タイプ | JaLC | |||||
著者 |
Usui, Yusuke
× Usui, Yusuke× Hiramatsu, Yoshihiro× Furumoto, Muneyoshi× Kanao, Masaki |
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著者別表示 |
臼井, 佑介
× 臼井, 佑介× 平松, 良浩× 古本, 宗充× 金尾, 政紀 |
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提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 情報・システム研究機構(ROIS)新領域融合研究センター(TRIC) | |||||
提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学大学院自然科学研究科 | |||||
提供者所属 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 金沢大学理学部 | |||||
書誌情報 |
Geophysical Research Letters 巻 32, 号 13, p. 1-4, 発行日 2005-07-16 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0094-8276 | |||||
DOI | ||||||
関連タイプ | isVersionOf | |||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.1029/2005GL022622 | |||||
出版者 | ||||||
出版者 | American Geophysical Union (AGU) | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Waveform modeling and travel times analyses of S, ScS and SKS phases recorded at the broad-band permanent station SYO in the Antarctic are used to determine the shear wave velocity structure and transverse isotropy in the D″ layer beneath the Antarctic Ocean. The SH wave structure has a discontinuity with the velocity increase of 2.0% at 2550 km. The SV structure is similar to PREM model. The magnitude of the anisotropy is highest at the top of D″ layer and lowest at the core-mantle boundary. The D″ layer beneath the Antarctic Ocean is significantly thicker than those beneath Alaska and the Caribbean Sea. We attribute this anisotropic D″ layer to paleo-slab materials. The subduction in and around the Antarctic Ocean has started ∼180 Ma and is the one of the oldest in the world. It has provided a large amount of the slab materials in the lowermost mantle. Copyright 2005 by the American Geophysical Union. | |||||
著者版フラグ | ||||||
出版タイプ | AM | |||||
出版タイプResource | http://purl.org/coar/version/c_ab4af688f83e57aa |