Dynamic conditions for large shallow intraslab earthquakes: four categories of subduction zones
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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1 Online-Ressource.
- Language
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Englisch
- Bibliographic citation
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Dynamic conditions for large shallow intraslab earthquakes: four categories of subduction zones ; volume:11 ; number:1 ; day:9 ; month:10 ; year:2024 ; pages:1-11 ; date:12.2024
Geoscience Letters ; 11, Heft 1 (9.10.2024), 1-11, 12.2024
- Creator
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Yoshida, Masaki
- Contributor
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SpringerLink (Online service)
- DOI
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10.1186/s40562-024-00361-7
- URN
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urn:nbn:de:101:1-2412262109553.062679154403
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:31 AM CEST
Data provider
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Associated
- Yoshida, Masaki
- SpringerLink (Online service)
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Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes
Frictional properties of sediments entering the Costa Rica subduction zone offshore the Osa Peninsula: implications for fault slip in shallow subduction zones
Halogens and trace elements in subduction zones
Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes
Geological evidence for shallow ductile-brittle transition zones along subduction interfaces: example from the Shimanto Belt, SW Japan
Shallow subduction zones, Pt. 1
Shallow subduction zones, Pt. 2
Seismogenic and tsunamigenic processes in shallow subduction zones
The link between great earthquakes and the subduction of oceanic fracture zones
Subduction zones, Pt. 1
Subduction zones, Pt. 2
Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone
Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes
Frictional properties of sediments entering the Costa Rica subduction zone offshore the Osa Peninsula: implications for fault slip in shallow subduction zones
Halogens and trace elements in subduction zones
Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes