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  1. 紀要論文
  2. 琉球大学理学部紀要
  3. 78号
  1. 部局別インデックス
  2. 理学部

Paleostress transition by fault-striation analysis in the northern and central Ryukyu arc, southwest Japan

http://hdl.handle.net/20.500.12000/2614
http://hdl.handle.net/20.500.12000/2614
fa9377f2-bde9-42b4-9fca-d4f9519ac7cb
名前 / ファイル ライセンス アクション
No78p163-2.pdf No78p163-2.pdf
No78p163-1.pdf No78p163-1.pdf
Item type デフォルトアイテムタイプ(フル)(1)
公開日 2008-03-27
タイトル
タイトル Paleostress transition by fault-striation analysis in the northern and central Ryukyu arc, southwest Japan
言語 en
作成者 Teramae, Noriaki

× Teramae, Noriaki

en Teramae, Noriaki

Hayashi, Daigoro

× Hayashi, Daigoro

en Hayashi, Daigoro

林, 大五郎

× 林, 大五郎

ja 林, 大五郎

アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
内容記述
内容記述タイプ Other
内容記述 The Ryukyu arc is an active arc-trench system, associate with active intracontinental back-arc basin (Okinawa Trough). Rifting of the Okinawa Trough has occurred since Miocene. The Ryukyu arc is expected to undergo complex geological history. Paleostress fields of the central and northern Ryukyu island are estimated from fault analysis by use of the Multi-inverse method (Yamaji, 2000) and Ginkgo method (Yamaji, 2003a).\nThe stress transition since middle Miocene is found by measurement of the fault-slip data in the northern and central Ryukyu arc. The fault-striation analysis leads the following tectonic evolution in the central and northern Ryukyu arc.\nIn middle Miocene, E-W extension occurred in the northern Ryukyu arc, which may be related to the opening of the Japan Sea. The compressional stress field occurred in late Miocene to early Pliocene (5-8 Ma), which was simultaneous with the formation of the Taiwan-Shinji Fold Belt. Subsequently E-W extension occurred in Pliocene, which was related to the opening the Okinawa Trough. Around at 2 Ma, complex stress regime occurred in the Ryukyu arc. In this time, opening of the Okinawa Trough resumed and the deposition of the Ryukyu group started. In northern Ryukyu arc, strike-slip stress regime has occurred from 2 Ma ago. NE-SW extension, arc-parallel extension is the latest stress regime in the central and northern Ryukyu arc. Arc parallel extension is observed in the whole Ryukyu arc. On the other hand, before the deposition of the Ryukyu group, stress regime of the southern Ryukyu arc is different from the central and northern Ryukyu arc.
内容記述タイプ Other
内容記述 紀要論文
出版者
言語 ja
出版者 琉球大学理学部
言語
言語 eng
資源タイプ
資源タイプ departmental bulletin paper
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
出版タイプ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
識別子
識別子 http://hdl.handle.net/20.500.12000/2614
識別子タイプ HDL
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 02869-640
収録物識別子タイプ NCID
収録物識別子 AN00250774
収録物名
言語 ja
収録物名 琉球大学理学部紀要
書誌情報
号 78, p. 163-231
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