4.8 Article

Mega-earthquakes rupture flat megathrusts

Journal

SCIENCE
Volume 354, Issue 6315, Pages 1027-1031

Publisher

AMER ASSOC ADVANCEMENT SCIENCE
DOI: 10.1126/science.aag0482

Keywords

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Funding

  1. NSF [EAR-1520238]
  2. ANR project TO-EOS
  3. French Ministry of Research and Education
  4. Division Of Earth Sciences
  5. Directorate For Geosciences [1520238] Funding Source: National Science Foundation

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The 2004 Sumatra-Andaman and 2011 Tohoku-Oki earthquakes highlighted gaps in our understanding of mega-earthquake rupture processes and the factors controlling their global distribution: A fast convergence rate and young buoyant lithosphere are not required to produce mega-earthquakes. We calculated the curvature along the major subduction zones of the world, showing that mega-earthquakes preferentially rupture flat (low-curvature) interfaces. A simplified analytic model demonstrates that heterogeneity in shear strength increases with curvature. Shear strength on flat megathrusts is more homogeneous, and hence more likely to be exceeded simultaneously over large areas, than on highly curved faults.

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