The Malawi Rift is localized within Precambrian amphibolite‐granulite facies metamorphic belts, bounded by up to 150 km long border faul...
Damaging aftershock sequences often exhibit considerable spatio‐temporal complexity. The stress changes associated with coseismic slip and as...
Aseismic afterslip has been proposed to drive aftershock sequences. Both afterslip moment and aftershock number broadly increase with mainshock siz...
The ability to estimate the likelihood of given earthquake magnitudes is critical for seismic hazard assessment. Earthquake magnitude‐recurre...
This work links mineral‐scale deformation mechanisms with structural evolution during subduction, providing examples showing how grain‐...
Geophysical observations indicate that patches of localized fracturing occur within otherwise viscous regions of subduction plate boundaries. These...