CORDIS Project
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This project investigates the mechanisms of earthquake generation by studying fault behavior in rocks under various conditions. Using advanced imaging techniques, it aims to understand the transition between slow and rapid slip, providing insights that could lead to improved earthquake prediction methods.
Deformation in Earth’s crust localizes onto faults that may rupture rapidly producing earthquakes or undergo slow aseismic slip.
The detailed mechanisms that control the transition between the seismic and aseismic regimes and the onset of earthquakes remain unknown.
These mechanisms control the geophysical processes preceding catastrophic failure, such as fracture development and strain localization on faults and in the rock volumes surrounding them.
Our goal is to provide the first quantitative…
UNIVERSITETET I OSLO
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INSTALLATION EUROPEENNE DE RAYONNEMENT SYNCHROTON
France, Grenoble
Type: Research institute
Activity type: Research Organisations
SME: No
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