scispace - formally typeset
S

Seiichi Miura

Researcher at Japan Agency for Marine-Earth Science and Technology

Publications -  99
Citations -  2607

Seiichi Miura is an academic researcher from Japan Agency for Marine-Earth Science and Technology. The author has contributed to research in topics: Trench & Subduction. The author has an hindex of 24, co-authored 96 publications receiving 2222 citations.

Papers
More filters
Journal ArticleDOI

Subducted seamount imaged in the rupture zone of the 1946 Nankaido earthquake

TL;DR: This work used densely deployed ocean bottom seismographs to detect a subducted seamount and proposes that this seamount might work as a barrier inhibiting brittle seismogenic rupture.
Journal ArticleDOI

Coseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquake

TL;DR: In this paper, images of the subduction trench next to the Tohoku-oki epicentre, captured using seismic reflection data 11 days after the 2011 earthquake, indicate that fault slip did reach the sea floor.
Journal ArticleDOI

Along-arc structural variation of the plate boundary at the Japan Trench margin: Implication of interplate coupling

TL;DR: In this paper, two kinds of interplate sedimentary units, a wedge-shaped unit and a channel-like unit, have been found to have a lower P wave velocity than the basal part of the overriding island arc crust.
Journal ArticleDOI

Structural factors controlling the rupture process of a megathrust earthquake at the Nankai trough seismogenic zone

TL;DR: In this paper, a subducting seamount at the centre of the proposed rupture zone with dimensions of 13 km thick by 50 km wide at 10 km depth was found and the seismic velocity image also showed that the seamount is now colliding with the Japanese island arc crust.
Journal ArticleDOI

Crustal structure across the coseismic rupture zone of the 1944 Tonankai earthquake, the central Nankai Trough seismogenic zone

TL;DR: In this article, the authors investigated differences in deep crustal structures of the rupture zones between the 1944 and 1946 Nankaido earthquakes and showed that the coseismic rupture extends to the Neogene-Quaternary accretionary prism.