The long recurrence intervals of small repeating earthquakes may be due to the slow slip rates of small fault strands
Observations since 1998 have revealed that repeating earthquakes, and particularly small repeating earthquakes, occur less often than expected given their seismically derived slip and the regional fault slip rate. Here we test the hypothesis that small repeaters occur infrequently because they occur...
| Main Authors: | , , |
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| Format: | Journal article |
| Published: |
American Geophysical Union
2019
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