Subduction of thick oceanic plateau and high‐angle normal‐fault earthquakes intersecting the slab-Reference-Cited by-同舟云学术

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Subduction of thick oceanic plateau and high‐angle normal‐fault earthquakes intersecting the slab

Published:2017-06-28 Issue:12 Volume:44 Page:6109-6115
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Arai Ryuta¹^ORCID,Kodaira Shuichi¹^ORCID,Yamada Tomoaki²,Takahashi Tsutomu¹^ORCID,Miura Seiichi¹,Kaneda Yoshiyuki³,Nishizawa Azusa⁴,Oikawa Mitsuhiro⁴

Affiliation:

1. Research and Development Center for Earthquake and Tsunami Japan Agency for Marine‐Earth Science and Technology Yokohama Japan

2. Earthquake Research Institute University of Tokyo Tokyo Japan

3. Institute of Education, Research and Regional Cooperation for Crisis Management Shikoku Kagawa University Takamatsu Japan

4. Hydrographic and Oceanographic Department Japan Coast Guard Tokyo Japan

Funder

Japanese Ministry of Education, Culture, Sports, Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL073789

Reference25 articles.

1. Structure of the tsunamigenic plate boundary and low-frequency earthquakes in the southern Ryukyu Trench

2. Crustal structure of the southern Okinawa Trough: Symmetrical rifting, submarine volcano, and potential mantle accretion in the continental back‐arc basin

3. Geologically current motion of 56 plates relative to the no-net-rotation reference frame

4. Thrust-type subduction-zone earthquakes and seamount asperities: A physical model for seismic rupture

5. Constraining fault friction in oceanic lithosphere using the dip angles of newly-formed faults at outer rises

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4. Intraslab Seismicity Migration Simultaneously with an Interface Slow Slip Event Along the Ecuadorian Subduction Zone;2024

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