Intermediate magnitude postseismic slip follows intermediate‐magnitude (M 4 to 5) earthquakes in California
<p style="text-align:justify;"> 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 cen...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
| Published: |
Wiley
2019
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