Accretionary prism deformation and fluid migration caused by slow earthquakes in the Nankai subduction zone
<p>Slow earthquakes induce structural deformation around their source regions and can also be linked to fluid migrations. Both of these phenomena potentially induce temporal variations in the seismic structure; how these two factors behave for a slow earthquake episode remains unknown. In this...
Saved in:
| Main Authors: | T. Tonegawa, T. Akuhara, Y. Yamashita, H. Sugioka, M. Shinohara, S. Takemura, T. Tsuji |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-06-01
|
| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/16/579/2025/se-16-579-2025.pdf |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Topography of the subducting basement throughout the entire Nankai Trough
by: Kazuya Shiraishi, et al.
Published: (2025-07-01) -
Enhanced deep learning approach for detecting and locating tectonic tremors in the Nankai subduction zone
by: Yuya Jinde, et al.
Published: (2025-07-01) -
Hydrocarbon seepage and its sources at mud volcanoes of the Kumano forearc basin, Nankai Trough subduction zone
by: Thomas Pape, et al.
Published: (2014-06-01) -
Crosscorrelation of Earthquake Data Using Stationary Phase Evaluation: Insight into Reflection Structures of Oceanic Crust Surface in the Nankai Trough
by: Shohei Minato, et al.
Published: (2012-01-01) -
GEOCHRONOLOGY OF THE METAMORPHIC ROCKS IN THE KURAI ACCRETIONARY PRISM (SOUTH-EASTERN GORNY ALTAI)
by: A. V. Kulikova, et al.
Published: (2017-12-01)