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Geological Origin of the Volcanic Islands of the Caroline Group in the Federated States of Micronesia, Western Pacific
http://hdl.handle.net/10232/17198
http://hdl.handle.net/10232/171983e8a52a8-bcba-4afa-a31b-de530cf8d6d8
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
AN10088628_v33n2_p101-118.pdf (1.3 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
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| 公開日 | 2014-11-14 | |||||
| タイトル | ||||||
| タイトル | Geological Origin of the Volcanic Islands of the Caroline Group in the Federated States of Micronesia, Western Pacific | |||||
| 言語 | en | |||||
| 著者 |
Rehman, Hafiz Ur
× Rehman, Hafiz Ur× 仲谷, 英夫× 河合, 渓 |
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| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | age | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | the Caroline Islands | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | hot-spot | |||||
| キーワード | ||||||
| 言語 | en | |||||
| 主題Scheme | Other | |||||
| 主題 | plate motion volcanics | |||||
| 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 | |||||
| 要約(Abstract) | ||||||
| 内容記述タイプ | Other | |||||
| 内容記述 | We present a geological review of the volcanic islands of the Caroline Islands group (Yap, Chuuk, Pohnpei and Kosrae) of the Federated States of Micronesia, to understand the origin and mechanism of formation of these volcanic islands. Previous geochronological data from the three volcanic islands (Chuuk: 14.8 to 4.3 Ma; Pohnpei: 8.7 to 0.92; and Kosrae: 2 to 1 Ma), indicate a progressive increase in age towards west, based on which a hot-spot origin was assigned. However, overlap in age of the volcanic islands and the absence of a hot spot east of Kosrae suggest involvement of other tectonic activity for their formation besides the simple hot-spot model. By observing geological features in the field (e.g., occurrence of structurally younger dikes which cross-cut the older volcanic sequences, presence of extensive dikes with columnar joints; indicative of extensional environment) and literature survey, we consider that the Caroline volcanic islands were not only remnants of a hot spot trace; as generally agreed by many authors, but were also produced in a fracture-induced subduction-related tectonic environment. |
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| 言語 | en | |||||
| 収録雑誌名 |
ja : 南太平洋研究 en : South Pacific Study 巻 33, 号 2, p. 101-118, 発行日 2013-03-29 |
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| 作成日 | ||||||
| 日付 | 2013-03-29 | |||||
| 日付タイプ | Issued | |||||
| ISSN | ||||||
| 収録物識別子タイプ | PISSN | |||||
| 収録物識別子 | 09160752 | |||||
| NII書誌ID（雑誌） | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN10088628 | |||||
| 出版タイプ | ||||||
| 出版タイプ | VoR | |||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
| NDC | ||||||
| 主題Scheme | NDC | |||||
| 主題 | 450 | |||||
| 公開者・出版者 | ||||||
| 出版者 | 鹿児島大学 | |||||
| 言語 | ja | |||||
| 公開者・出版者 | ||||||
| 出版者 | Kagoshima University | |||||
| 言語 | en | |||||
