Size and duration of the high-frequency radiator in the source of the 2004 December 26 Sumatra earthquake

Geophysical Journal International

Volumn 170, Issue 3, 2007, Pages 1119-1128

  Gusev, A A ^a,b   Guseva, E M ^b   Panza, G F ^c  

^a INSTITUTE OF VOLCANOLOGY AND SEISMOLOGY   (Russian Federation)

^b Kamchatka Branch   (Russian Federation)

^c UNIVERSITY OF TRIESTE   (Italy)

Author keywords

Earthquake source mechanism; Rupture propagation; Seismic coda; Source time functions; Subduction zone; Waveform analysis

Indexed keywords

AFTERSHOCK; CODA; DATA INVERSION; EARTHQUAKE RUPTURE; GREEN FUNCTION; P-WAVE; SOURCE PARAMETERS; SUBDUCTION ZONE; SUMATRA EARTHQUAKE 2004; TELESEISMIC WAVE; WAVEFORM ANALYSIS;

EID: 34548139432     PISSN: 0956540X     EISSN: 1365246X     Source Type: Journal    
DOI: 10.1111/j.1365-246X.2007.03368.x     Document Type: Article

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