Spatio-temporal source characteristics of the 26 December 2004 Sumatra earthquake as imaged by teleseismic broadband arrays

2005 ◽  
Vol 32 (24) ◽  
Author(s):  
F. Krüger ◽  
M. Ohrnberger
Keyword(s):  
Sumatra Earthquake ◽  
Source Characteristics ◽  
2004 Sumatra Earthquake ◽  
Spatio Temporal

Seismic evidence for broken oceanic crust in the 2004 Sumatra earthquake epicentral region

2008 ◽  
Vol 1 (11) ◽  
pp. 777-781 ◽  
Author(s):  
Satish C. Singh ◽  
Hélène Carton ◽  
Paul Tapponnier ◽  
Nugroho D. Hananto ◽  
Ajay P. S. Chauhan ◽  
...  
Keyword(s):  
Oceanic Crust ◽  
Sumatra Earthquake ◽  
2004 Sumatra Earthquake ◽  
Epicentral Region

A splash in Earth gravity from the 2004 Sumatra Earthquake

Eos ◽  
2005 ◽  
Vol 86 (15) ◽  
pp. 149 ◽  
Author(s):  
Roberto Sabadini ◽  
Giorgio Dalla Via ◽  
Masja Hoogland ◽  
Abdelkrim Aoudia
Keyword(s):  
Sumatra Earthquake ◽  
Earth Gravity ◽  
2004 Sumatra Earthquake

The 1755 Lisbon earthquake and the beginning of closure of the Atlantic

2006 ◽  
Vol 14 (2) ◽  
pp. 193-205 ◽  
Author(s):  
A. RIBEIRO ◽  
L. MENDES-VICTOR ◽  
J. CABRAL ◽  
L. MATIAS ◽  
P. TERRINHA
Keyword(s):  
Source Area ◽  
Accretionary Prism ◽  
Sumatra Earthquake ◽  
Alert System ◽  
Tsunami Modelling ◽  
2004 Sumatra Earthquake ◽  
Lisbon Earthquake ◽  
History Of ◽  
History Of Europe ◽  
Gorringe Bank

The 1755 Lisbon earthquake and tsunami had one of the highest magnitudes in the history of Europe. The source mechanism requires generation at a subduction zone. Intensity distribution and tsunami modelling excludes the Gorringe Bank as a source area and suggests generation by the incipient convergence of the Atlantic with the Southwest Iberia and Morocco margin rather than at the less active Gulf of Cadiz Accretionary Prism. The comparison with the 2004 Sumatra earthquake and tsunami supports this interpretation. A tsunami warning alert system is urgent for the Atlantic.

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