Exploring the relationship between stress state and fault stability at the Hikurangi Subduction Margin, New Zealand

The Hikurangi Subduction Margin (HSM), New Zealand is characterized by along-strike variation in slip behavior, thought to be linked to spatial-temporal variations of plate interface coupling, tectonic stresses, and pore pressures in the overriding pl

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Publication Details

Published
2025-10-02
DOI
https://doi.org/10.22541/essoar.175941865.57646398/v1
Primary Topic
Geological and Geophysical Studies
Type
article
Field-Weighted Citation Impact
0.00

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article

Exploring the relationship between stress state and fault stability at the Hikurangi Subduction Margin, New Zealand

Ivan Lokmer, Effat Behboudi, David D. McNamara
Geological and Geophysical Studies
article

Exploring the relationship between stress state and fault stability at the Hikurangi Subduction Margin, New Zealand

Ivan Lokmer, Effat Behboudi, David D. McNamara
article en

Abstract

The Hikurangi Subduction Margin (HSM), New Zealand is characterized by along-strike variation in slip behavior, thought to be linked to spatial-temporal variations of plate interface coupling, tectonic stresses, and pore pressures in the overriding pl

University College Dublin (IE), University of Liverpool (GB), Centre de Géosciences (FR)
Science Foundation Ireland
Openalex Percentile: Top 63%
Geological and Geophysical Studies
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