Impacts of Hikurangi Plateau subduction on the origin and evolution of the Alpine Fault
Author:
Affiliation:
1. Tectonophysics Department, GNS Science, Lower Hutt, New Zealand
Funder
Royal Society of New Zealand
Marsden Fund
Publisher
Informa UK Limited
Subject
Earth and Planetary Sciences (miscellaneous),Geology,Geophysics
Link
https://www.tandfonline.com/doi/pdf/10.1080/00288306.2018.1454481
Reference77 articles.
1. Focal mechanisms of large earthquakes in the South Island of New Zealand: implications for the accommodation of Pacific-Australia plate motion
2. Focal mechanisms and inter-event times of low-frequency earthquakes reveal quasi-continuous deformation and triggered slow slip on the deep Alpine Fault
3. New c. 270 kyr strike-slip and uplift rates for the southern Alpine Fault and implications for the New Zealand plate boundary
4. Major Earthquakes Occur Regularly on an Isolated Plate Boundary Fault
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