Abstract:Large earthquakes rupture faults over hundreds of kilometers within
minutes. Finite-fault models elucidate these processes and provide
observational constraints for understanding earthquake physics. However,
finite-fault inversions are subject to non-uniqueness and substantial
uncertainties. The diverse range of published models for the
well-recorded 2011 M_w 9.0 Tohoku-Oki earthquake aptly illustrates this
issue, and details of its rupture process remain under debate. Here, we
comprehensively compare 32 finit… Show more
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