Structural Characteristics of the Nankai Trough Shallow Plate Boundary Inferred From Shallow Very Low Frequency Earthquakes-Reference-Cited by-同舟云学术

Structural Characteristics of the Nankai Trough Shallow Plate Boundary Inferred From Shallow Very Low Frequency Earthquakes

Published:2019-04-17 Issue:8 Volume:46 Page:4192-4201
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Takemura Shunsuke¹²^ORCID,Matsuzawa Takanori¹^ORCID,Noda Akemi¹^ORCID,Tonegawa Takashi³^ORCID,Asano Youichi¹^ORCID,Kimura Takeshi¹^ORCID,Shiomi Katsuhiko¹^ORCID

Affiliation:

1. National Research Institute for Earth Science and Disaster Resilience Tsukuba Japan

2. Now at Earthquake Research InstituteThe University of Tokyo Tokyo Japan

3. Japan Agency for Marine‐Earth Science and Technology Yokohama Japan

Funder

Japan Society for the Promotion of Science

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL082448

Reference69 articles.

1. Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan

2. Shallow episodic tremor near the Nankai Trough axis off southeast Mie prefecture, Japan

3. Recurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrust

4. Spatiotemporal distribution of very-low frequency earthquakes in Tokachi-oki near the junction of the Kuril and Japan trenches revealed by using array signal processing

5. Possible shallow slow slip events in Hyuga-nada, Nankai subduction zone, inferred from migration of very low frequency earthquakes

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