Fluid upwelling across the Hikurangi subduction thrust during deep slow-slip earthquakes

to related objects

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: 1 Online-Ressource.

Language: Englisch

Bibliographic citation: Fluid upwelling across the Hikurangi subduction thrust during deep slow-slip earthquakes ; volume:5 ; number:1 ; day:12 ; month:11 ; year:2024 ; pages:1-8 ; date:12.2024
Communications earth & environment ; 5, Heft 1 (12.11.2024), 1-8, 12.2024

Creator: Herath, Pasan
Audet, Pascal

Contributor: SpringerLink (Online service)

DOI: 10.1038/s43247-024-01864-z

URN: urn:nbn:de:101:1-2501292147093.693628321578

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:27 AM CEST

Data provider

This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.

Show original at data provider

Associated

Herath, Pasan
Audet, Pascal
SpringerLink (Online service)

Other Objects (12)

Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust

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

Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes

Integrated rupture mechanics for slow slip events and earthquakes

Scaling of characterized slip models for plate-boundary earthquakes

Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Correction to: Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

Width of surface rupture zone for thrust earthquakes: implications for earthquake fault zoning

Width of surface rupture zone for thrust earthquakes. Implications for earthquake fault zoning.

Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust

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

Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes

Integrated rupture mechanics for slow slip events and earthquakes

Scaling of characterized slip models for plate-boundary earthquakes

Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Correction to: Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

Width of surface rupture zone for thrust earthquakes: implications for earthquake fault zoning

Width of surface rupture zone for thrust earthquakes. Implications for earthquake fault zoning.

Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust

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

Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes

Integrated rupture mechanics for slow slip events and earthquakes

Scaling of characterized slip models for plate-boundary earthquakes

Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Correction to: Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

Width of surface rupture zone for thrust earthquakes: implications for earthquake fault zoning

Width of surface rupture zone for thrust earthquakes. Implications for earthquake fault zoning.

Cultural heritage institutions wishing to register will find more information here.

Fields marked * need to be filled in.

Username*

Please enter your username

Email*

Please enter your email address

Please do not fill this field

First name

Last name

Password*

Please enter your password

Confirm password*

Please enter the same password

I have read the terms of use and the privacy policy for the collection of personal data and accept them. *

This field is required.

I would like to subscribe to the newsletter of the Deutsche Digitale Bibliothek. See newsletter subscription info.

Account created

Your "My DDB" account has been successfully created. Before you can log in to your account, you must click the confirmation link in the message we just sent to the email address you provided.

Fluid upwelling across the Hikurangi subduction thrust during deep slow-slip earthquakes

Object Details

References and Relationships

Contributors, Places and Time

Further information

Data provider

Associated

Other Objects (12)

Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust

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

Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes

Integrated rupture mechanics for slow slip events and earthquakes

Scaling of characterized slip models for plate-boundary earthquakes

Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Correction to: Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

Width of surface rupture zone for thrust earthquakes: implications for earthquake fault zoning

Width of surface rupture zone for thrust earthquakes. Implications for earthquake fault zoning.

Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust

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

Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes

Integrated rupture mechanics for slow slip events and earthquakes

Scaling of characterized slip models for plate-boundary earthquakes

Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Correction to: Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

Width of surface rupture zone for thrust earthquakes: implications for earthquake fault zoning

Width of surface rupture zone for thrust earthquakes. Implications for earthquake fault zoning.

Seasonal modulation of deep slow-slip and earthquakes on the Main Himalayan Thrust

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

Heterogeneous slab thermal dehydration driving warm subduction zone earthquakes

Integrated rupture mechanics for slow slip events and earthquakes

Scaling of characterized slip models for plate-boundary earthquakes

Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

The Saint-Ursanne earthquakes of 2000 revisited: evidence for active shallow thrust-faulting in the Jura fold-and-thrust belt

Mantle upwelling induced by slab rollover subduction could explain widespread intraplate volcanism in Tibet

Correction to: Stress state along the western Nankai Trough subduction zone inferred from b-values, long-term slow-slip events, and low-frequency earthquakes

Width of surface rupture zone for thrust earthquakes: implications for earthquake fault zoning

Width of surface rupture zone for thrust earthquakes. Implications for earthquake fault zoning.

Related objects

Reset password