Asymmetric Brittle Deformation at the Pāpaku Fault, Hikurangi Subduction Margin, NZ, IODP Expedition 375-Reference-Cited by-同舟云学术

Asymmetric Brittle Deformation at the Pāpaku Fault, Hikurangi Subduction Margin, NZ, IODP Expedition 375

Published:2021-08 Issue:8 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Savage Heather M.¹^ORCID,Shreedharan Srisharan²³^ORCID,Fagereng Åke⁴^ORCID,Morgan Julia K.⁵,Meneghini Francesca⁶^ORCID,Wang Maomao⁷^ORCID,McNamara David D.⁸^ORCID,Wallace Laura M.⁹³^ORCID,Saffer Demian M.²³,Barnes Philip M.¹⁰^ORCID,Petronotis Katerina E.¹¹^ORCID,LeVay Leah J.¹¹^ORCID

Affiliation:

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

2. Department of Geosciences The Pennsylvania University University Park PA USA

3. University of Texas Institute for Geophysics Austin TX USA

4. School of Earth & Ocean Sciences Cardiff University Cardiff UK

5. Department of Earth Sciences Rice University Houston TX USA

6. Dipartimento di Scienze della Terra Universita degli Studi di Pisa Pisa Italy

7. College of Oceanography Hohai University Nanjing China

8. Department of Earth, Ocean and Ecological Sciences University of Liverpool Liverpool UK

9. GNS Science Lower Hutt New Zealand

10. National Institute of Water and Atmospheric Research Wellington New Zealand

11. International Ocean Discovery Program Texas A&M University College Station TX USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009662

Reference57 articles.

1. Upper Limit on Damage Zone Thickness Controlled by Seismogenic Depth

2. Wrinkle-like slip pulse on a fault between different materials

3. Geophysical Constraints on the Relationship Between Seamount Subduction, Slow Slip, and Tremor at the North Hikurangi Subduction Zone, New Zealand

4. Slow slip source characterized by lithological and geometric heterogeneity

5. Hikurangi margin tsunami earthquake generated by slow seismic rupture over a subducted seamount

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4. Characterizing the porosity structure and gas hydrate distribution at the southern Hikurangi Margin, New Zealand from offshore electromagnetic data;Geophysical Journal International;2023-04-27

5. Seafloor overthrusting causes ductile fault deformation and fault sealing along the Northern Hikurangi Margin;Earth and Planetary Science Letters;2022-09