Earthquake Directivity, Orientation, and Stress Drop Within the Subducting Plate at the Hikurangi Margin, New Zealand-Reference-Cited by-同舟云学术

Earthquake Directivity, Orientation, and Stress Drop Within the Subducting Plate at the Hikurangi Margin, New Zealand

Published:2017-12 Issue:12 Volume:122 Page:10,176-10,188
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Abercrombie Rachel E.¹^ORCID,Poli Piero²^ORCID,Bannister Stephen³^ORCID

Affiliation:

1. Department of Earth and Environment; Boston University; Boston MA USA

2. Department of Earth; Atmospheric and Planetary Sciences, MIT; Cambridge MA USA

3. GNS Science; Lower Hutt New Zealand

Funder

Government of New Zealand

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JB014935/fullpdf

Reference43 articles.

1. Comparison of direct and coda wave stress drop measurements for the Wells, Nevada, earthquake sequence;Abercrombie;Journal of Geophysical Research: Solid Earth,2013

2. Stress drops of repeating earthquakes on the San Andreas Fault at Parkfield;Abercrombie;Geophysical Research Letters,2014

3. Investigating uncertainties in empirical Green's function analysis of earthquake source parameters;Abercrombie;Journal of Geophysical Research: Solid Earth,2015

4. Variability of earthquake stress drop in a subduction setting, the Hikurangi Margin, New Zealand;Abercrombie;Geophysical Journal International,2017

5. Uncertainty, variability, and earthquake physics in groundmotion prediction equations;Baltay;Bulletin of the Seismological Society of America,2017

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