http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/cruise/yokosuka/yk11-e05/ehttp://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-08/ehttp://www.godac.jamstec.go.jp/darwin/cruise/kaiyo/ky11-e05/ehttp://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr12-20/ehttp://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr13-01/ehttp://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr13-12/ehttp://www.godac.jamstec.go.jp/darwin/cruise/kaiyo/ky14-05/
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr14-e02/ehttp://www.godac.jamstec.go.jp/darwin/...
Abstract The Ryukyu (Nansei-Shoto) island arc-trench system, southwest of Japan, is formed by the su...
Seismic velocity structure of the mantle beneath Japan has been determined on the basis of teleseism...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
Subduction of the oceanic plate plays an important role in the various processes in subduction zones...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr09-06/ehttp://www.godac.jamstec.go.jp/darwin/c...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr99-08/ehttp://www.godac.jamstec.go.jp/darwin/c...
http://www.godac.jamstec.go.jp/darwin/cruise/kaimei/km20-05/ehttp://www.godac.jamstec.go.jp/darwin/c...
Abstract Devastating megathrust earthquakes and slow earthquakes both occur along subducting plate i...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr15-11_leg3/ehttp://www.godac.jamstec.go.jp/dar...
http://www.godac.jamstec.go.jp/darwin/cruise/kaiyo/ky12-02/ehttp://www.godac.jamstec.go.jp/darwin/cr...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr13-18/ehttp://www.godac.jamstec.go.jp/darwin/c...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr14-e02/ehttp://www.godac.jamstec.go.jp/darwin/...
Abstract The Ryukyu (Nansei-Shoto) island arc-trench system, southwest of Japan, is formed by the su...
Seismic velocity structure of the mantle beneath Japan has been determined on the basis of teleseism...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr11-e03/ehttp://www.godac.jamstec.go.jp/darwin/...
Subduction of the oceanic plate plays an important role in the various processes in subduction zones...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr09-06/ehttp://www.godac.jamstec.go.jp/darwin/c...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr99-08/ehttp://www.godac.jamstec.go.jp/darwin/c...
http://www.godac.jamstec.go.jp/darwin/cruise/kaimei/km20-05/ehttp://www.godac.jamstec.go.jp/darwin/c...
Abstract Devastating megathrust earthquakes and slow earthquakes both occur along subducting plate i...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr15-11_leg3/ehttp://www.godac.jamstec.go.jp/dar...
http://www.godac.jamstec.go.jp/darwin/cruise/kaiyo/ky12-02/ehttp://www.godac.jamstec.go.jp/darwin/cr...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr13-18/ehttp://www.godac.jamstec.go.jp/darwin/c...
http://www.godac.jamstec.go.jp/darwin/cruise/kairei/kr14-e02/ehttp://www.godac.jamstec.go.jp/darwin/...
Abstract The Ryukyu (Nansei-Shoto) island arc-trench system, southwest of Japan, is formed by the su...
Seismic velocity structure of the mantle beneath Japan has been determined on the basis of teleseism...