Strike‐Slip Enables Subduction Initiation Beneath a Failed Rift: New Seismic Constraints From Puysegur Margin, New Zealand

Author:

Shuck Brandon12ORCID,Van Avendonk Harm1ORCID,Gulick Sean P. S.12ORCID,Gurnis Michael3ORCID,Sutherland Rupert4ORCID,Stock Joann3ORCID,Patel Jiten4ORCID,Hightower Erin3ORCID,Saustrup Steffen1,Hess Thomas12

Affiliation:

1. Institute for Geophysics Jackson School of Geosciences University of Texas at Austin Austin TX USA

2. Department of Geological Sciences Jackson School of Geosciences University of Texas at Austin Austin TX USA

3. Seismological Laboratory California Institute of Technology Pasadena CA USA

4. School of Geography Environment and Earth Sciences Victoria University of Wellington Wellington New Zealand

Funder

National Science Foundation

FURTHERMORE grants in publishing

University of Texas at Austin

California Institute of Technology

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference118 articles.

1. The thermal structure of subduction zones constrained by seismic imaging: Implications for slab dehydration and wedge flow

2. Implications for extensional tectonics;Axen G. J.;Journal of Geophysical Research,1997

3. Seismic stratigraphic record of transition from Mesozoic subduction to continental breakup in the Zealandia sector of eastern Gondwana

4. Evolution of the Nankai Trough décollement from the trench into the seismogenic zone: Inferences from three‐dimensional seismic reflection imaging;Bangs N. L.;Geologica,2004

5. Basement geology of the Campbell Plateau: Implications for correlation of the Campbell Magnetic Anomaly System

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