From 3-Hz P Waves to ₀S₂: No Evidence of A Slow Component to the Source of the 2011 Tohoku Earthquake

Keyphrases

• Seismic Source 100%
• P-wave 100%
• Slow Component 100%
• 2011 Tohoku Earthquake 100%
• Chile 66%
• Nias 66%
• Sumatra 66%
• Scaling Laws 33%
• Tsunami 33%
• Mega 33%
• Peru 33%
• Spheroidal 33%
• Graves 33%
• Ultra-long 33%
• Seismic Moment 33%
• Tahiti 33%
• Tsunami Early Warning 33%
• Teleseismic 33%
• Subduction Events 33%
• Sendai 33%
• Slow Earthquake 33%
• Flat Spectrum 33%
• Phase Inversion 33%
• W Phase 33%
• Breathing Mode 33%
• Static Moment 33%
• Alaska 33%
• Tohoku Earthquake 33%
• Earthquake Information 33%
• Information Centres 33%
• Honshu 33%
• Source Scaling 33%
• Mentawai 33%
• Real-time Modeling 33%

Earth and Planetary Sciences

• Seismic Source 100%
• Tohoku Earthquake 2011 100%
• P Wave 100%
• Real Time 66%
• Chile 66%
• Seismic Moment 33%
• Scaling Law 33%
• Dichotomy 33%
• Information Centre 33%
• Peru 33%
• Alaska 33%