日本地球惑星科学連合2015年大会

講演情報

インターナショナルセッション(口頭発表)

セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT07] New constraints on the tectonic evolution of Northeast Asia

2015年5月25日(月) 11:00 〜 12:45 A03 (アパホテル&リゾート 東京ベイ幕張)

コンビーナ:*Jonny Wu(Department of Geosciences, National Taiwan University)、Kyoko Okino(Ocean Research Institute, University of Tokyo)、Cedric Legendre(Institute of Earth Sciences, Academia Sinica, Taiwan)、Gaku Kimura(Department of Earth and Planetary Science of the Graduate School of Science, The University of Tokyo)、座長:谷 健一郎(国立科学博物館地学研究部)、Lee Yuan Hsi(Department of Earth and Environmental Sciences, National CHung-Cheng University)

12:30 〜 12:33

[SIT07-P01] フィリピン海の発達史:大陸棚調査で得られた磁気異常データからの考察

ポスター講演3分口頭発表枠

*沖野 郷子1 (1.東京大学大気海洋研究所)

キーワード:テクトニクス, フィリピン海, 地磁気異常, 背弧海盆, 島弧

Marine magnetic anomalies have been used to date the seafloor, characterize the oceanic crust and reconstruct the evolution process of ocean basins. Japanese continental shelf survey project has collected high-quality, dense magnetic data in the Philippine Sea and the adjacent areas for two decades. The compiled and processed magnetic anomaly data improve our understanding of the tectonic history of the area. Clear magnetic lineation patterns in the Shikoku, Parece Vela basins allow us to elaborate the spreading history of these basins, including the initiation and cessation process of the backarc opening. The anomalies associated with the Kyushu-Palau Ridge also record the transitional phase from arc volcanism to backarc rifting-opening. The West Philippine Basin, Daito Ridges and its intervening small basins, that was formed before the formation of the paleo-IBM arc, show their specific magnetic characteristics. These areas are considered to have moved northward and rotated after their formation. The skewness analysis of magnetic data can provide us some insights about paleo-latitude and/or rotation.