New publication as a co-author on the following key points:
- The Mw7.8 Kaikōura earthquake was followed by local deformation at Taupō volcano, c. 500 km away
- The deformation observed is consistent with either a dike intrusion or aseismic slip on a fault
- Dynamic stress changes in the range of 0.15–0.9 MPa caused by seismic waves from the Kaikōura earthquake triggered this response at Taupō
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2023JB028585
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