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the devastating megathrust earthquake of 26 december 2004 was caused by the release of stresses that developed as the india plate subducted beneath the overriding burma plate.
el masivo y devastador terremoto del 26 de diciembre de 2004 tuvo su origen en la liberación de las fuerzas que fueron acumulándose a medida que la placa de la india iba deslizándose bajo la placa de birmania.
historically, great or giant megathrust earthquakes have been recorded in 1797, 1833, 1861, 2004, 2005 and 2007, most of them being associated with devastating tsunamis.
históricamente, los terremotos de mega impulso grandes o gigantes se han registrado en 1797, 1833, 1861, 2004, 2005 y 2007, la mayoría de ellos están asociados a tsunamis devastadores.
preliminary locations of larger aftershocks following the megathrust earthquake show that approximately 1200 km of the plate boundary slipped as a result of the earthquake.123 this was confirmed in a recent survey by the hms scott conducted in the exclusive economic zone of indonesia under the marine scientific research provisions of unclos.124
estas conclusiones se vieron confirmadas en una reciente investigación realizada por el buque hms scott en la zona económica exclusiva de indonesia según las disposiciones de la convención de las naciones unidas sobre el derecho del mar relativas a la investigación científica marina.
the megathrust earthquake involved the juan de fuca plate that underlies the pacific ocean, from mid-vancouver island in british columbia, canada, south along the pacific northwest coast as far as northern california.
en el terremoto estuvieron implicadas la placa de juan de fuca y la placa del pacífico, desde la isla de vancouver en canadá hasta la costa norte de california en estados unidos.
* katsushisa, k., masayuki, t., 2004, short-period seismic radiation zones of a megathrust fault along the nankai, trough deduced from inversion analysis of seismic intensity data, journal of seismilogical society of japan, v. 57, no.
* katsushisa, k., masayuki, t., 2004, short-period seismic radiation zones of a megathrust fault along the nankai, trough deduced from inversion analysis of seismic intensity data, journal of seismilogical society of japan, v. 57, no.
