Mixed Brittle and Viscous Strain Localization in Pelagic Sediments Seaward of the Hikurangi Margin, New Zealand-Reference-Cited by-同舟云学术

Mixed Brittle and Viscous Strain Localization in Pelagic Sediments Seaward of the Hikurangi Margin, New Zealand

Published:2020-08 Issue:8 Volume:39 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Leah Harold¹^ORCID,Fagereng Åke¹^ORCID,Meneghini Francesca²^ORCID,Morgan Julia K.³,Savage Heather M.⁴^ORCID,Wang Maomao⁵^ORCID,Bell Rebecca⁶,Ikari Matt J.⁷^ORCID

Affiliation:

1. School of Earth and Ocean Sciences Cardiff University Cardiff UK

2. Dipartimento di Scienze della Terra Universit degli Studi di Pisa Pisa Italy

3. Department of Earth Science Rice University Houston TX USA

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

5. College of Oceanography Hohai University Nanjing China

6. Basins Research Group Imperial College London London UK

7. MARUM Center for Marine Enviromental Sciences and Faculty of Geosciences University of Bremen Bremen Germany

Funder

Seventh Framework Programme

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019TC005965

Reference103 articles.

1. Interaction between pressure solution and clays in stylolite development: Insights from modeling

2. Thermal regime of the Northern Hikurangi Margin, New Zealand;Antriasian A.;Geophysical Journal International,2018

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

4. Geometry of the Hikurangi subduction thrust and upper plate, North Island, New Zealand

5. Slow slip source characterized by lithological and geometric heterogeneity

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3. Inherited Heterogeneities Can Control Viscous Subduction Zone Deformation of Carbonates at Seismogenic Depths;Geophysical Research Letters;2022-10-07

4. Plate‐Rate Frictional Behavior of Sediment Inputs to the Hikurangi Subduction Margin: How Does Lithology Control Slow Slip Events?;Geochemistry, Geophysics, Geosystems;2022-06

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