Geophysical Constraints on the Relationship Between Seamount Subduction, Slow Slip, and Tremor at the North Hikurangi Subduction Zone, New Zealand-Reference-Cited by-同舟云学术

Geophysical Constraints on the Relationship Between Seamount Subduction, Slow Slip, and Tremor at the North Hikurangi Subduction Zone, New Zealand

Published:2018-12-12 Issue:23 Volume:45 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Barker Daniel H. N.¹^ORCID,Henrys Stuart¹^ORCID,Caratori Tontini Fabio¹^ORCID,Barnes Philip M.²^ORCID,Bassett Dan¹^ORCID,Todd Erin³^ORCID,Wallace Laura¹⁴^ORCID

Affiliation:

1. GNS Science Lower Hutt New Zealand

2. National Institute of Water and Atmospheric Research Wellington New Zealand

3. Department of Geology University of Otago Dunedin New Zealand

4. Institute for Geophysics University of Texas Austin TX USA

Funder

Royal Society of New Zealand

Ministry of Business, Innovation and Employment

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018GL080259

Reference41 articles.

1. Geometry of the Hikurangi subduction thrust and upper plate, North Island, New Zealand

2. Slow wavespeeds and fluid overpressure in a region of shallow geodetic locking and slow slip, Hikurangi subduction margin, New Zealand

3. Hikurangi margin tsunami earthquake generated by slow seismic rupture over a subducted seamount

4. Seismic reflection character of the Hikurangi subduction interface, New Zealand, in the region of repeated Gisborne slow slip events

5. Slow Earthquakes and Nonvolcanic Tremor

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