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Paleomagnetic and K-Ar dating studies of Late Cretaceous basaltic dykes intruding Late Permian sediments of Newcastle Coal Measures,Newcastle, Australia-Relationship to the opening of the Tasman Sea
https://doi.org/10.15094/00003150
https://doi.org/10.15094/00003150976d2635-e8d4-4f0f-aad8-4d621e357a5f
名前 / ファイル | ライセンス | アクション |
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KJ00003562999 (1.5 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 2005-10-01 | |||||
タイトル | ||||||
タイトル | Paleomagnetic and K-Ar dating studies of Late Cretaceous basaltic dykes intruding Late Permian sediments of Newcastle Coal Measures,Newcastle, Australia-Relationship to the opening of the Tasman Sea | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Paleomagnetism, Late Cretaceous, Newcastle, Tasman Sea opening, VGP | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003150 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
論文名よみ | ||||||
その他のタイトル | Paleomagnetic and K-Ar dating studies of Late Cretaceous basaltic dykes intruding Late Permian sediments of Newcastle Coal Measures,Newcastle, Australia-Relationship to the opening of the Tasman Sea | |||||
著者名(英) |
Sakai,Hideo
× Sakai,Hideo× Kikawa,Eiichi× Offle,Robin× Zwingmann,Horst |
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著者所属(英) | ||||||
en | ||||||
Department of Earth Sciences, Toyama University/Independent Administrative Institution, Japan Agency for Marine-Earth Science and Technology/Discipline of Earth Sciences, University of Newcastle/CSIRO Petroleum, Bentley | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | Paleomagnetic studies of Late Cretaceous basaltic dykes (K-Ar age of ca. 80Ma) and associated sediments reveal the presence of both normal and reverse polarity magnetizations. Correlation with the geomagnetic polarity time scale shows that the normal polarity magnetization could have been acquired in the geomagnetic polarity chron (C33n) and the reversed polarity magnetization may have been acquired in the C33r or C32r polarity chron, respectively. This indicates that pulses of magmatism occurred in the region over a substantial period. The normal and reverse magnetic directions show a clockwise deflection from the north-south direction of 40-50°, which may be related to block rotation associated with deformation events that have occurred subsequent to dyke emplacement or to the opening of the Tasman Sea. | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 18, p. 58-66, 発行日 2005-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |