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Intermediate magnitude postseismic slip follows intermediate‐magnitude (M 4 to 5) earthquakes in California

Abstract:

The magnitude of postseismic slip is useful for constraining physical models of fault slip. Here we examine the postseismic slip following intermediate‐magnitude (M 4 to 5) earthquakes by systematically analyzing data from borehole strainmeters in central and northern California. We assess the noise in the data and identify 11 earthquakes that generated interpretable strain records. We estimate the earthquakes' postseismic to coseismic moment ratios by compari...

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Publication status:
Published
Peer review status:
Peer reviewed

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Files:
Publisher copy:
10.1029/2018gl081001

Authors


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Role:
Author
ORCID:
0000-0002-8396-8513
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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Oxford college:
St Cross College
Role:
Author
ORCID:
0000-0002-4117-2082
Publisher:
Wiley Publisher's website
Journal:
Geophysical Research Letters Journal website
Volume:
46
Issue:
7
Pages:
3676-3687
Publication date:
2019-04-04
Acceptance date:
2019-03-15
DOI:
EISSN:
1944-8007
ISSN:
0094-8276
Language:
English
Keywords:
Pubs id:
pubs:983615
UUID:
uuid:6a2c235d-2416-4c44-ba08-347b8be0d26c
Local pid:
pubs:983615
Source identifiers:
983615
Deposit date:
2019-03-21

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