The epicentre was located 90 km south of Sinabang with 30 Km Depth 2.065 N 97.010 E; Evidence emerges that earthquake generated significant tsunami. Any queries (other than missing content) should be directed to the corresponding author for the article.Please check your email for instructions on resetting your password. Physics, Astrophysics and AstronomyI have read and accept the Wiley Online Library Terms and Conditions of UseRupture process of the 2004 Sumatra‐Andaman earthquakeThe size and duration of the Sumatra‐Andaman earthquake from far‐field static offsetsEffect of recent revisions to the geomagnetic reversal time‐scale on estimates of current plate motionsDetermination of earthquake source parameters from waveform data for studies of global and regional seismicityEarthquake source parameters and stress distribution in the Adak Island region of the central Aleutian Islands, AlaskaGlobal seismicity of 2003: Centroid‐moment‐tensor solutions for 1087 earthquakesRupture extent, duration, and speed of the 2004 Sumatra‐Andaman earthquake imaged by the Hi‐Net arraySource characteristics of the great Sumatra earthquake and its aftershocksEarth's free oscillations excited by the 26 December 2004 Sumatra‐Andaman earthquakeInsight into the 2004 Sumatra‐Andaman earthquake from GPS measurements in 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In the twenty-four hours immediately after the event, there were eight major aftershocks, measuring between 5.5 and 6.0.
Station RAYN lies roughly in the direction of rupture propagation. Please note: The publisher is not responsible for the content or functionality of any supporting information supplied by the authors.
The Northern Sumatra Earthquake of March 28, 2005 Editor’s Note: Beginning with the March issue and in each one sub-sequently, we presented six reports by the many teams that observed the effects of the December 26, 2004, earthquake and tsunami in countries around the Indian Ocean. (1896-1977)International The even arrivals (major arc and subsequent orbits) are enhanced in amplitude.
The March 28, 2005, M 8.6 northern Sumatra, Indonesia, earthquake occurred as the result of thrust faulting on the interface of the Australia plate and Sunda plate and was caused by the release of stresses that develop as the Australia plate subducts beneath the overriding Sunda plate.
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