The Role of Metamorphic Fluid in Tectonic Tremor Along the Alpine Fault, New Zealand
Author:
Affiliation:
1. School of Environmental and Rural Science University of New England Armidale NSW Australia
2. School of Geography, Environment and Earth Sciences Victoria University of Wellington Wellington New Zealand
Funder
University of New England
Victoria University of Wellington
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL096415
Reference67 articles.
1. Source mechanism of a lower crust earthquake beneath the Himalayas and its possible relation to metamorphism
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. The tectonic evolution of the Southern Alps, New Zealand: insights from fully thermally coupled dynamical modelling
4. Episodic Tremor and Slip Explained by Fluid‐Enhanced Microfracturing and Sealing
5. Peak metamorphic temperature and thermal history of the Southern Alps (New Zealand)
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