Constraints on rupture of the December 26, 2004, Sumatra earthquake from far-field GPS observations

[1]  Matthias Ohrnberger,et al.  Tracking the rupture of the Mw = 9.3 Sumatra earthquake over 1,150 km at teleseismic distance , 2005, Nature.

[2]  J. Curray,et al.  Tectonics and history of the Andaman Sea region , 2005 .

[3]  Ó. Gudmundsson,et al.  GPS analyses of the Sumatra-Andaman earthquake , 2005 .

[4]  Emile A. Okal,et al.  Seismology: Speed and size of the Sumatra earthquake , 2005, Nature.

[5]  H. Kanamori,et al.  The Great Sumatra-Andaman Earthquake of 26 December 2004 , 2005, Science.

[6]  T. Fitch Plate convergence, transcurrent faults, and internal deformation adjacent to Southeast Asia and the western Pacific , 1972 .

[7]  K. Sieh Aceh–Andaman earthquake: What happened and what's next? , 2005, Nature.

[8]  F. Pollitz,et al.  The Size and Duration of the Sumatra-Andaman Earthquake from Far-Field Static Offsets , 2005, Science.

[9]  Shamita Das,et al.  Fine details of the Wadati-Benioff zone under Indonesia and its geodynamic implications , 1999 .

[10]  Y. Okada Internal deformation due to shear and tensile faults in a half-space , 1992, Bulletin of the Seismological Society of America.

[11]  Chen Ji,et al.  Rupture Process of the 2004 Sumatra-Andaman Earthquake , 2005, Science.

[12]  S. Jade,et al.  Co-seismic and post-seismic displacements in Andaman and Nicobar Islands from GPS measurements , 2005 .

[13]  H. Kanamori,et al.  Seismology: Energy radiation from the Sumatra earthquake , 2005, Nature.

[14]  Peter M. Shearer,et al.  Extent, duration and speed of the 2004 Sumatra–Andaman earthquake imaged by the Hi-Net array , 2005, Nature.

[15]  R. Bilham,et al.  Partial and Complete Rupture of the Indo-Andaman Plate Boundary 1847-2004 , 2005 .

[16]  Pierre Henry,et al.  The Sumatra subduction zone: A case for a locked fault zone extending into the mantle , 2004 .

[17]  Jeroen Tromp,et al.  Earth's Free Oscillations Excited by the 26 December 2004 Sumatra-Andaman Earthquake , 2005, Science.