From Earthquake Centroid to Spatial-Temporal Rupture Evolution: Mw 6.3 Movri Mountain Earthquake, June 8, 2008, Greece

Abstract

A new slip inversion method is introduced, being based on back projection of residual seismograms. The method enabled to reveal a delayed asperity from recordings of the Mw 6.3 Movri Mountain Earthquake, June 8, 2008, Greece

Keywords

• Earthquake
• Centroid
• Spatial-Temporal
• Rupture
• Evolution
• Movri
• Mountain
• Earthquake
• Greece