Author Correction: High probability of successive occurrence of Nankai megathrust earthquakes
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- ISSN
-
2045-2322
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Anmerkungen
-
online resource.
- Erschienen in
-
Author Correction: High probability of successive occurrence of Nankai megathrust earthquakes ; volume:13 ; number:1 ; day:3 ; month:2 ; year:2023 ; pages:1-2 ; date:12.2023
Scientific reports ; 13, Heft 1 (3.2.2023), 1-2, 12.2023
- Urheber
-
Fukushima, Yo
Nishikawa, Tomoaki
Kano, Yasuyuki
- Beteiligte Personen und Organisationen
-
SpringerLink (Online service)
- DOI
-
10.1038/s41598-023-29306-4
- URN
-
urn:nbn:de:101:1-2023040809100926003011
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
14.08.2025, 11:01 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Fukushima, Yo
- Nishikawa, Tomoaki
- Kano, Yasuyuki
- SpringerLink (Online service)
Ähnliche Objekte (12)
Link between the Nankai underthrust turbidites and shallow slow earthquakes
A review of shallow slow earthquakes along the Nankai Trough
Error propagation in time-dependent probability of occurrence for characteristic earthquakes in Italy
A b map implying the first eastern rupture of the Nankai Trough earthquakes
Simulation of great earthquakes along the Nankai Trough: reproduction of event history, slip areas of the Showa Tonankai and Nankai earthquakes, heterogeneous slip-deficit rates, and long-term slow slip events
Scaling Analysis of Time Distribution between Successive Earthquakes in Aftershock Sequences
Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone
Amplification of tsunami heights by delayed rupture of great earthquakes along the Nankai trough
Three-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off Kumano
What controls the occurrence of shallow intraplate earthquakes?
Accretionary prism deformation and fluid migration caused by slow earthquakes in the Nankai subduction zone
Buried large block revealed by gravity anomalies in the Tonankai and Nankai earthquakes regions, southwestern Japan
Link between the Nankai underthrust turbidites and shallow slow earthquakes
A review of shallow slow earthquakes along the Nankai Trough
Error propagation in time-dependent probability of occurrence for characteristic earthquakes in Italy
A b map implying the first eastern rupture of the Nankai Trough earthquakes
Simulation of great earthquakes along the Nankai Trough: reproduction of event history, slip areas of the Showa Tonankai and Nankai earthquakes, heterogeneous slip-deficit rates, and long-term slow slip events
Scaling Analysis of Time Distribution between Successive Earthquakes in Aftershock Sequences
Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone
Amplification of tsunami heights by delayed rupture of great earthquakes along the Nankai trough
Three-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off Kumano
What controls the occurrence of shallow intraplate earthquakes?
Accretionary prism deformation and fluid migration caused by slow earthquakes in the Nankai subduction zone
Buried large block revealed by gravity anomalies in the Tonankai and Nankai earthquakes regions, southwestern Japan
Link between the Nankai underthrust turbidites and shallow slow earthquakes
A review of shallow slow earthquakes along the Nankai Trough
Error propagation in time-dependent probability of occurrence for characteristic earthquakes in Italy
A b map implying the first eastern rupture of the Nankai Trough earthquakes
Simulation of great earthquakes along the Nankai Trough: reproduction of event history, slip areas of the Showa Tonankai and Nankai earthquakes, heterogeneous slip-deficit rates, and long-term slow slip events
Scaling Analysis of Time Distribution between Successive Earthquakes in Aftershock Sequences
Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone
Amplification of tsunami heights by delayed rupture of great earthquakes along the Nankai trough
Three-dimensional topographic relief of the oceanic crust may control the occurrence of shallow very-low-frequency earthquakes in the Nankai Trough off Kumano
What controls the occurrence of shallow intraplate earthquakes?
Accretionary prism deformation and fluid migration caused by slow earthquakes in the Nankai subduction zone