Dataciencia

Colección SciELO Chile

The occurrence and hazards of great subduction zone earthquakes

Indexado

WoS	WOS:000743864200001
Scopus	SCOPUS_ID:85122890218

DOI

10.1038/S43017-021-00245-W

Año

2022

Tipo

revisión

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras

Abstract

Some of the most devastating natural hazards on Earth are caused by subduction zone earthquakes. This Review discusses the conditions required to generate M >= 8 megathrust earthquakes, in the context of constraining seismic and tsunami hazards.

Revista

Revista	ISSN
	2662-138X

Métricas Externas

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Disciplinas de Investigación

WOS
Sin Disciplinas

Scopus
Sin Disciplinas

SciELO
Sin Disciplinas

Muestra la distribución de disciplinas para esta publicación.

Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional

Muestra la distribución de colaboración, tanto nacional como extranjera, generada en esta publicación.

Autores - Afiliación

Ord.	Autor	Género	Institución - País
1	Wirth, Erin A.	Mujer	US GEOL SURVEY - Estados Unidos United States Geological Survey - Estados Unidos
2	Sahakian, Valerie J.	Mujer	UNIV OREGON - Estados Unidos University of Oregon - Estados Unidos
3	Wallace, L.	Mujer	GNS Sci - Nueva Zelanda Univ Texas Austin - Estados Unidos GNS Science - Nueva Zelanda Jackson School of Geosciences - Estados Unidos
4	Melnick, Daniel	Hombre	Universidad Austral de Chile - Chile

Muestra la afiliación y género (detectado) para los co-autores de la publicación.

Financiamiento

Fuente
FONDECYT
Fondo Nacional de Desarrollo Científico y Tecnológico
Millennium Scientific Initiative
National Aeronautics and Space Administration
Institut de Cardiologie de Montréal
Millennium Scientific Initiative (ICM) of the Chilean government
NASA ROSES
ANID
ANID PIA Anillo

Muestra la fuente de financiamiento declarada en la publicación.

Agradecimientos

Agradecimiento
The authors thank G. Hayes and J. Gomberg for helpful and constructive feedback, which helped to improve this manuscript. V.J.S. was supported, in part, by NASA ROSES grant 80NSSC21K0841. D.M. was supported by the Millennium Scientific Initiative (ICM) of the Chilean government through grant NC160025 'Millennium Nucleus CYCLO The Seismic cycle along subduction zones', FONDECYT grants 1181479 and 1190258, and the ANID PIA Anillo ACT192169.
The authors thank G. Hayes and J. Gomberg for helpful and constructive feedback, which helped to improve this manuscript. V.J.S. was supported, in part, by NASA ROSES grant 80NSSC21K0841. D.M. was supported by the Millennium Scientific Initiative (ICM) of the Chilean government through grant NC160025 ‘Millennium Nucleus CYCLO The Seismic cycle along subduction zones’, FONDECYT grants 1181479 and 1190258, and the ANID PIA Anillo ACT192169.

Agradecimiento

The authors thank G. Hayes and J. Gomberg for helpful and constructive feedback, which helped to improve this manuscript. V.J.S. was supported, in part, by NASA ROSES grant 80NSSC21K0841. D.M. was supported by the Millennium Scientific Initiative (ICM) of the Chilean government through grant NC160025 'Millennium Nucleus CYCLO The Seismic cycle along subduction zones', FONDECYT grants 1181479 and 1190258, and the ANID PIA Anillo ACT192169.

The authors thank G. Hayes and J. Gomberg for helpful and constructive feedback, which helped to improve this manuscript. V.J.S. was supported, in part, by NASA ROSES grant 80NSSC21K0841. D.M. was supported by the Millennium Scientific Initiative (ICM) of the Chilean government through grant NC160025 ‘Millennium Nucleus CYCLO The Seismic cycle along subduction zones’, FONDECYT grants 1181479 and 1190258, and the ANID PIA Anillo ACT192169.