Abstract
In many subduction zones in the world, low-frequency tremors and earthquakes have been recognized at a depth of about 30 km. They occur independently or migrate along the trench direction of the plate interface. We investigate behaviors of their patterns through numerical simulation, by varying frictional properties of the plate interface. Our simulation results indicate that a chain reaction of small asperities can reproduce the migration process in terms of the migration speedand the slip velocity, under the condition that characteristicslip distance is larger than 0.4 mm.
Original language | English |
---|---|
Title of host publication | Advances in Geosciences |
Subtitle of host publication | Volume 26: Solid Earth (SE) |
Publisher | World Scientific Publishing Co. |
Pages | 47-54 |
Number of pages | 8 |
ISBN (Electronic) | 9789814355391 |
ISBN (Print) | 9814355380, 9789814355384 |
DOIs | |
Publication status | Published - 2011 Jan 1 |
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Engineering(all)
- Environmental Science(all)