Low dissipation of earthquake energy along faults that follow pre-existing weaknesses: field and microstructural observations of Malawi's Bilila-Mtakataka Fault
2021
Fracturing and gouge formation absorb ≥50% of earthquake energy on low displacement (<1-2 km) faults in isotropic crust. To assess how these processes absorb earthquake energy in anisotropic crust,...
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