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Slow earthquakes triggered by typhoons
ChiChing Liu1, Alan T Linde, I Selwyn Sacks
1Institute for Earth Sciences, Academica Sinica, 128 Sinica Road, Sec. 2, Nankang, Taipei 115, Taiwan, China. liucc@sinica.edu.tw
Nature
|June 12, 2009
Summary
Typhoons can trigger slow earthquakes in eastern Taiwan. These slow slip events may segment fault zones, potentially inhibiting larger seismic ruptures in this highly deformed region.
Area of Science:
- Geophysics
- Seismology
- Tectonics
Background:
- Slow earthquakes, characterized by gradual seismic slip, have been documented globally.
- The potential for slow earthquakes to trigger ordinary earthquakes is an area of ongoing research.
- Understanding earthquake triggering mechanisms is crucial for seismic hazard assessment.
Purpose of the Study:
- To investigate the triggering of slow earthquakes by typhoons in eastern Taiwan.
- To model the physical processes governing typhoon-induced slow earthquakes.
- To assess the role of slow earthquakes in modulating seismic activity in compressional tectonic settings.
Main Methods:
- Analysis of seismic data from eastern Taiwan.
- Numerical modeling of slow slip events on a reverse fault.
- Investigation of fault mechanics under varying pressure conditions.
Main Results:
- Slow earthquakes in eastern Taiwan were found to be triggered by typhoons.
- Modeling indicated that reduced fault pressure, caused by typhoons, can initiate slow slip.
- The studied slow earthquakes occurred as repeated episodes of slow slip on a west-dipping reverse fault.
Conclusions:
- Typhoons can act as triggers for slow earthquakes by reducing fault pressure.
- Repeating slow earthquakes may play a role in segmenting seismically active areas.
- This segmentation could inhibit the occurrence of large earthquakes in regions with high compressional deformation.
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