13,500+ fault segments from GEM database with slip rates. ALL earthquakes - micro to major. Deep quakes (>300km) reveal lower mantle structure near LLSVPs.
π¬ Building Stress Model...Loading GEM fault database...
Deep quakes (>300km) occur in subducting slabs and help "image" the lower mantle near LLSVPs like seismic tomography.
Note: Parallel fault lines are separate strands in the GEM database. Major fault zones (like the San Andreas) contain multiple parallel segments. Colors indicate stress level based on slip rate and recent seismic activity.