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Tidal synchronicity of the 26 December 2004 Sumatran earthquake and its aftershocks
Author(s) -
Crockett R. G. M.,
Gillmore G. K.,
Phillips P. S.,
Gilbertson D. D.
Publication year - 2006
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2006gl027074
Subject(s) - seismology , geology , foreshock , aftershock , period (music) , trench , earthquake swarm , remotely triggered earthquakes , tsunami earthquake , induced seismicity , chemistry , physics , organic chemistry , layer (electronics) , acoustics
The frequency of earthquake incidence along the Andaman/Sunda/Java Trench plate‐boundary region has been investigated for the ten‐lunar‐month period 28 October 2004–19 August 2005, encompassing the 26 December 2004 earthquake. During this period variations in earthquake activity correlate with the tidal‐force cycles: maxima in earthquake activity occur around the times of new and full moons, typically lagging by 0–3 days. This relationship is consistent with earthquake inducement via ocean tidal loading. Also, during this period the earthquake incidence associated with new and full moons at the western end of the region was (a) 38% and (b) 86% higher than the period averages for the full and declustered major‐earthquake catalogs respectively.