CORDIS Project
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This project investigates slow earthquakes, a type of fault movement that is faster than creeping but slower than traditional earthquakes. By analyzing various fault structures and deformation mechanisms, it aims to develop numerical models that enhance understanding of fault behavior and the potential for seismic acti…
Major tectonic faults have, until recently, been thought to accommodate displacement by either continuous creep or episodic, damaging earthquakes.
High-resolution geophysical networks have now detected ‘slow earthquakes’, transient modes of displacement that are faster than creep but slower than earthquakes.
This project aims to illuminate the unknown mechanism behind slow earthquakes, through an integrated, multi-scale approach. MICA uses the unique natural laboratory of exhumed and active faul…
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