Temporal Relationship of Slow Slip Events and Microearthquake Seismicity: Insights From Earthquake Automatic Detections in the Northern Hikurangi Margin, Aotearoa New Zealand

Temporal Relationship of Slow Slip Events and Microearthquake Seismicity: Insights From Earthquake Automatic Detections in the Northern Hikurangi Margin, Aotearoa New Zealand

Abstract Slow slip events in the northern Hikurangi margin of Aotearoa New Zealand occur every 18–24 months and last for several weeks before returning to average convergence rates of around 38 mm/yr. Along this plate boundary, the Hikurangi plateau subducts beneath the overlying Australian plate an...

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Bibliographic Details
Main Authors: Jefferson Yarce, Anne F. Sheehan, Steven Roecker
Format: Article
Language:English
Published: Wiley 2023-03-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Hikurangi
slow slip event
earthquake detection
seismicity
subduction
ocean bottom seismometers
Online Access:https://doi.org/10.1029/2022GC010537

Internet

https://doi.org/10.1029/2022GC010537

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