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Characteristics of relocated hypocenters of the 2018 M6.7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three-dimensional seismic velocity structure

Earth, planets, and space, 2019-11, Vol.71 (1), p.1-11, Article 122

Kita, Saeko

2019

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Physical mechanisms of oceanic mantle earthquakes: Comparison of natural and experimental events

Scientific reports, 2018-11, Vol.8 (1), p.17049-11, Article 17049

2018

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Effects of episodic slow slip on seismicity and stress near a subduction-zone megathrust

Nature communications, 2021-12, Vol.12 (1), p.7253-7253, Article 7253

2021

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Stress drops of intermediate-depth intraslab earthquakes beneath Tohoku, northern Japan

Earth, planets, and space, 2024-12, Vol.76 (1), p.84-16, Article 84

2024

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Stress drops for intermediate-depth intraslab earthquakes beneath Hokkaido, northern Japan: Differences between the subducting oceanic crust and mantle events

Geochemistry, geophysics, geosystems : G3, 2015-02, Vol.16 (2), p.552-562

2015

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Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials

Earth and planetary science letters, 2010-02, Vol.290 (3), p.415-426

2010

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Special issue “The 2018 Hokkaido Eastern Iburi Earthquake and Hidaka arc–arc collision system”

Earth, planets, and space, 2020-05, Vol.72 (1), p.1-3, Article 65

2020

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High-resolution seismic velocity structure beneath the Hokkaido corner, northern Japan: Arc-arc collision and origins of the 1970 M 6.7 Hidaka and 1982 M 7.1 Urakawa-oki earthquakes

Journal of Geophysical Research: Solid Earth, 2012-12, Vol.117 (B12), p.n/a

2012

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Temporal variation of intermediate‐depth earthquakes around the time of the M9.0 Tohoku‐oki earthquake

Geophysical research letters, 2017-04, Vol.44 (8), p.3580-3590

2017

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Existence of interplane earthquakes and neutral stress boundary between the upper and lower planes of the double seismic zone beneath Tohoku and Hokkaido, northeastern Japan

Tectonophysics, 2010-12, Vol.496 (1), p.68-82

2010

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Existence of a seismic belt in the upper plane of the double seismic zone extending in the along-arc direction at depths of 70–100 km beneath NE Japan

Geophysical research letters, 2006-12, Vol.33 (24), p.L24310-n/a

2006

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Tomographic imaging of hydrated crust and mantle in the subducting Pacific slab beneath Hokkaido, Japan: Evidence for dehydration embrittlement as a cause of intraslab earthquakes

Gondwana research, 2009-12, Vol.16 (3), p.470-481

2009

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Dynamic rupture simulation of the 2011 off the Pacific coast of Tohoku Earthquake: Multi-event generation within dozens of seconds

Earth, planets, and space, 2013-01, Vol.64 (12), p.1167-1175

2013

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Detailed seismic attenuation structure beneath Hokkaido, northeastern Japan: Arc-arc collision process, arc magmatism, and seismotectonics

Journal of geophysical research. Solid earth, 2014-08, Vol.119 (8), p.6486-6511

2014

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Anomalous deepening of a belt of intraslab earthquakes in the Pacific slab crust under Kanto, central Japan: Possible anomalous thermal shielding, dehydration reactions, and seismicity caused by shallower cold slab material

Geophysical research letters, 2007-05, Vol.34 (9), p.L09305-n/a

2007

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Large intraslab earthquake (2011 April 7, M 7.1) after the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0): Coseismic fault model based on the dense GPS network data

Earth, planets, and space, 2011-01, Vol.63 (12), p.1207-1211

2011

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Stress drops for intermediate‐depth intraslab earthquakes beneath H okkaido, northern J apan: Differences between the subducting oceanic crust and mantle events

Geochemistry, geophysics, geosystems : G3, 2015-02, Vol.16 (2), p.552-562

2015

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Seismic attenuation structure associated with episodic tremor and slip zone beneath Shikoku and the Kii peninsula, southwestern Japan, in the Nankai subduction zone

Journal of geophysical research. Solid earth, 2016-03, Vol.121 (3), p.1962-1982

2016

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The 2005 M7.2 MIYAGI-OKI earthquake, NE Japan: Possible rerupturing of one of asperities that caused the previous M7.4 earthquake

Geophysical research letters, 2005-12, Vol.32 (24), p.L24302-n/a

2005

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Depth variations in seismic velocity in the subducting crust: Evidence for fluid‐related embrittlement for intermediate‐depth earthquakes

Geophysical research letters, 2017-01, Vol.44 (2), p.810-817

2017

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Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake

Geophysical research letters, 2011-04, Vol.38 (7), p.n/a

2011

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A weak subducting slab at intermediate depths below northeast Japan

Science advances, 2024-03, Vol.10 (9), p.eadh2106-eadh2106

2024

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Temporal variation of intermediate‐depth earthquakes around the time of the M 9.0 Tohoku‐oki earthquake

Geophysical research letters, 2017-04, Vol.44 (8), p.3580-3590

2017

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Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake

Geophysical research letters, 2012, Vol.39 (7)

2012

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Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake: HYDRATED FAULT AND INTRASLAB EARTHQUAKES

Geophysical research letters, 2011-04, Vol.38 (7), p.n/a

2011

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Characteristics of relocated hypocenters of the 2018 M6.7 Hokkaido Eastern Iburi earthquake and its aftershocks with a three-dimensional seismic velocity structure

Physical mechanisms of oceanic mantle earthquakes: Comparison of natural and experimental events

Effects of episodic slow slip on seismicity and stress near a subduction-zone megathrust

Stress drops of intermediate-depth intraslab earthquakes beneath Tohoku, northern Japan

Stress drops for intermediate-depth intraslab earthquakes beneath Hokkaido, northern Japan: Differences between the subducting oceanic crust and mantle events

Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials

Special issue “The 2018 Hokkaido Eastern Iburi Earthquake and Hidaka arc–arc collision system”

High-resolution seismic velocity structure beneath the Hokkaido corner, northern Japan: Arc-arc collision and origins of the 1970 M 6.7 Hidaka and 1982 M 7.1 Urakawa-oki earthquakes

Temporal variation of intermediate‐depth earthquakes around the time of the M9.0 Tohoku‐oki earthquake

Existence of interplane earthquakes and neutral stress boundary between the upper and lower planes of the double seismic zone beneath Tohoku and Hokkaido, northeastern Japan

Existence of a seismic belt in the upper plane of the double seismic zone extending in the along-arc direction at depths of 70–100 km beneath NE Japan

Tomographic imaging of hydrated crust and mantle in the subducting Pacific slab beneath Hokkaido, Japan: Evidence for dehydration embrittlement as a cause of intraslab earthquakes

Dynamic rupture simulation of the 2011 off the Pacific coast of Tohoku Earthquake: Multi-event generation within dozens of seconds

Detailed seismic attenuation structure beneath Hokkaido, northeastern Japan: Arc-arc collision process, arc magmatism, and seismotectonics

Anomalous deepening of a belt of intraslab earthquakes in the Pacific slab crust under Kanto, central Japan: Possible anomalous thermal shielding, dehydration reactions, and seismicity caused by shallower cold slab material

Large intraslab earthquake (2011 April 7, M 7.1) after the 2011 off the Pacific coast of Tohoku Earthquake (M 9.0): Coseismic fault model based on the dense GPS network data

Stress drops for intermediate‐depth intraslab earthquakes beneath H okkaido, northern J apan: Differences between the subducting oceanic crust and mantle events

Seismic attenuation structure associated with episodic tremor and slip zone beneath Shikoku and the Kii peninsula, southwestern Japan, in the Nankai subduction zone

The 2005 M7.2 MIYAGI-OKI earthquake, NE Japan: Possible rerupturing of one of asperities that caused the previous M7.4 earthquake

Depth variations in seismic velocity in the subducting crust: Evidence for fluid‐related embrittlement for intermediate‐depth earthquakes

Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake

A weak subducting slab at intermediate depths below northeast Japan

Temporal variation of intermediate‐depth earthquakes around the time of the M 9.0 Tohoku‐oki earthquake

Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake

Seismic evidence for reactivation of a buried hydrated fault in the Pacific slab by the 2011 M9.0 Tohoku earthquake: HYDRATED FAULT AND INTRASLAB EARTHQUAKES

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