Observations of Laboratory and Natural Slow Slip Events: Hikurangi Subduction Zone, New Zealand-Reference-Cited by-同舟云学术

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Observations of Laboratory and Natural Slow Slip Events: Hikurangi Subduction Zone, New Zealand

Published:2020-02 Issue:2 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Ikari Matt J.¹^ORCID,Wallace Laura M.²³^ORCID,Rabinowitz Hannah S.⁴^ORCID,Savage Heather M.⁵^ORCID,Hamling Ian J.²^ORCID,Kopf Achim J.¹

Affiliation:

1. MARUM Center for Marine Environmental Sciences and Faculty of Geosciences University of Bremen Bremen Germany

2. GNS Science Lower Hutt New Zealand

3. Institute for Geophysics University of Texas Austin TX USA

4. Department of Earth, Environmental, and Planetary Sciences Brown University Providence RI USA

5. Department of Earth and Planetary Sciences University of California, Santa Cruz Santa Cruz CA USA

Funder

Deutsche Forschungsgemeinschaft

H2020 European Research Council

European Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GC008717

Reference98 articles.

1. Time-dependent modeling of slow slip events and associated seismicity and tremor at the Hikurangi subduction zone, New Zealand

2. Slow wavespeeds and fluid overpressure in a region of shallow geodetic locking and slow slip, Hikurangi subduction margin, New Zealand

3. Strength of Strained Two‐Phase Mixtures: Application to Rapid Creep and Stress Amplification in Subduction Zone Mélange

4. Seismic reflection character of the Hikurangi subduction interface, New Zealand, in the region of repeated Gisborne slow slip events

5. Critical evaluation of state evolution laws in rate and state friction: Fitting large velocity steps in simulated fault gouge with time‐, slip‐, and stress‐dependent constitutive laws

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1. Clay-rich fault gouges become frictionally less stable at elevated temperatures;2024-08-05

2. Macro and micro connections for slip zone soils of landslide under wetting–drying cycles in the Three Gorges Reservoir area;Landslides;2024-01-03

3. Characteristics of Slow Slip Events Explained by Rate‐Strengthening Faults Subject to Periodic Pore Fluid Pressure Changes;Journal of Geophysical Research: Solid Earth;2023-06

4. Effects of phyllosilicate content on the slip behavior of fault gouge: Insights from room-temperature friction experiments on quartz–talc mixtures;Tectonophysics;2023-06

5. Ultralow frictional healing explains recurring slow slip events;Science;2023-02-17

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