Porosity and Compaction State at the Active Pāpaku Thrust Fault in the Frontal Accretionary Wedge of the North Hikurangi Margin-Reference-Cited by-同舟云学术

Porosity and Compaction State at the Active Pāpaku Thrust Fault in the Frontal Accretionary Wedge of the North Hikurangi Margin

Published:2021-10 Issue:10 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Dutilleul Jade¹²^ORCID,Bourlange S.¹^ORCID,Géraud Y.¹

Affiliation:

1. GeoRessources CNRS University of Lorraine Nancy France

2. Now at Earthquake Research Institute The University of Tokyo Tokyo Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009325

Reference134 articles.

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3. Temporal Variations in Crustal Scattering Structure near Parkfield, California, Using Receiver Functions

4. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing

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

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1. Permeability and Elastic Properties of Rocks From the Northern Hikurangi Margin: Implications for Slow‐Slip Events;Geophysical Research Letters;2024-01-23

2. Effective Porosity Profile at IODP Site C0002 in the Heart of the Nankai Accretionary Prism, and Its Use for Predicting In Situ Seismic Velocities;Geophysical Research Letters;2023-02-14

3. Porosity and permeability evolution in the Tuaheni Landslide Complex at Hikurangi margin from IODP Sites U1517 and U1519;New Zealand Journal of Geology and Geophysics;2021-10-25