- Abstract:
-
The low frequency earthquakes (LFEs) that constitute tectonic tremor are often inferred to be slow: to have durations of 0.2 to 0.5 s, a factor of 10 to 100 longer than those of typical MW 1-2 earthquakes. Here we examine LFEs near Parkfield, CA in order to assess several proposed explanations for LFEs’ long durations. We determine LFE rupture areas and location distributions using a new approach, similar to directivity analysis, where we examine how signals coming from various locations with...
Expand abstract - Publication status:
- Published
- Peer review status:
- Peer reviewed
- Version:
- Accepted Manuscript
- Files:
-
-
(pdf, 3.4mb)
-
- Publisher copy:
- 10.1093/gji/ggy429
-
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- Publisher:
- Oxford University Press Publisher's website
- Journal:
- Geophysical Journal International Journal website
- Volume:
- 216
- Issue:
- 1
- Pages:
- 621–639
- Publication date:
- 2018-10-13
- Acceptance date:
- 2018-10-11
- DOI:
- EISSN:
-
1365-246X
- ISSN:
-
0956-540X
- Pubs id:
-
pubs:929744
- URN:
-
uri:8ba9c4a5-63e3-4642-a779-d96e013d18c9
- UUID:
-
uuid:8ba9c4a5-63e3-4642-a779-d96e013d18c9
- Local pid:
- pubs:929744
- Copyright holder:
- Hawthorne et al.
- Copyright date:
- 2018
- Notes:
-
Copyright © 2018 The Authors. Published by Oxford University Press on behalf of The Royal Astronomical Society. This is the accepted manuscript version of the article. The final version is available online from Oxford University Press at: https://doi.org/10.1093/gji/ggy429
Journal article
The rupture extent of low frequency earthquakes near Parkfield, CA
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