Additional file 1 Additional figures showing enlarged MCS profiles with interpretation and OBS record sections for forward modeling
Abstract In this study, which was conducted to investigate present-day geological deformations occur...
The relations between the frequency of occurrence and the magnitude of earthquakes are established i...
Structures beneath back-arc basins or marginal seas are as important as those beneath island arcs an...
Abstract The Okinawa Trough, to the southwest of Kyusyu, Japan, is an active backarc basin of the Ry...
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/kr13-18/ehttp://www.godac.jamstec.go.jp/darwin/c...
Abstract The southern part of the Okinawa Trough forms a narrow back-arc rift basin where evidence f...
International audienceThe Okinawa Trough, lying to the east of China, is a back arc basin formed by ...
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/kr13-18/ehttp://www.godac.jamstec.go.jp/darwin/c...
Abstract Tectonic and volcanic structures of the northern Ryukyu arc are investigated on the basis o...
Abstract. The Okinawa Trough, lying between Japan and Taiwan, is a backarc basin formed by extension...
Abstract The Ryukyu (Nansei-Shoto) island arc-trench system, southwest of Japan, is formed by the su...
Additional file 1: Figure S1. Frequency–magnitude distributions of earthquakes in the southern Okina...
The Okinawa Trough, lying between Japan and Taiwan, is a backarc basin formed by extension within th...
Abstract In this study, which was conducted to investigate present-day geological deformations occur...
The relations between the frequency of occurrence and the magnitude of earthquakes are established i...
Structures beneath back-arc basins or marginal seas are as important as those beneath island arcs an...
Abstract The Okinawa Trough, to the southwest of Kyusyu, Japan, is an active backarc basin of the Ry...
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/kr13-18/ehttp://www.godac.jamstec.go.jp/darwin/c...
Abstract The southern part of the Okinawa Trough forms a narrow back-arc rift basin where evidence f...
International audienceThe Okinawa Trough, lying to the east of China, is a back arc basin formed by ...
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/kr13-18/ehttp://www.godac.jamstec.go.jp/darwin/c...
Abstract Tectonic and volcanic structures of the northern Ryukyu arc are investigated on the basis o...
Abstract. The Okinawa Trough, lying between Japan and Taiwan, is a backarc basin formed by extension...
Abstract The Ryukyu (Nansei-Shoto) island arc-trench system, southwest of Japan, is formed by the su...
Additional file 1: Figure S1. Frequency–magnitude distributions of earthquakes in the southern Okina...
The Okinawa Trough, lying between Japan and Taiwan, is a backarc basin formed by extension within th...
Abstract In this study, which was conducted to investigate present-day geological deformations occur...
The relations between the frequency of occurrence and the magnitude of earthquakes are established i...
Structures beneath back-arc basins or marginal seas are as important as those beneath island arcs an...
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