Long-term seismic observations along Myanmar–Sunda subduction margin: insights for 2004 Mw > 9.0 earthquake

  • Prosanta Kumar Khan
  • Jayashree Banerjee
  • Sk Shamim
  • Manoranjan Mohanty
Original Paper
  • 33 Downloads

Abstract

The present study investigates the temporal variation of few seismic parameters between the Myanmar (Zone I), Andaman–Nicobar–Northwest Sumatra (Zone II), Southeast Sumatra–West Indonesia (Zone III) and East Indonesia (Zone IV) converging boundaries in reference to the generation of 26 December 2004 Mw > 9.0 off-Sumatra mega-earthquake event. The four segments are distinguished based on tectonics parameters, distinct geological locations, great earthquake occurrences, and the Wadati–Benioff zone characteristics. Two important seismic parameters such as seismic energy and b values are computed over a time-window of 6-month period during the entire 1976–2013 period for these segments. The b values show a constant decrease in Zones II, III, and IV, whereas the Zone I does not show any such pattern prior to the 2004 mega-event. The release of seismic energy was also gradually decreasing in Zones II and III till the 2004 event, and little similar pattern was also noted in Zone IV. This distinct observation might be indicating that the stress accumulation was dominant near the Sumatra–Java area located towards southeast of Zone II and northwest of Zone III. The released strain energy during the 2004 event was subsequently migrated towards north, rupturing ~ 1300 km of the boundary between the Northwest Sumatra and the North Andaman. The occurrence of 2004 mega-event was apparently concealed behind the long-term seismic quiescence existing near the Sumatra and Nicobar margin. A systematic study of the patterns of seismic energy release and b values, and the long-term observation of collective behaviour of the margin tectonics might have had given clues to the possibility of the 2004 mega-event.

Keywords

Myanmar–Sunda margin 2004 Mw 9.3 mega-earthquake Seismic b value Seismic energy pattern Seismic quiescence 

Notes

Acknowledgements

First author is thankful to the Director, Indian Institute of Technology (ISM), Dhanbad, for providing the infrastructure facilities. This work has been supported by the grants of the Department of Science and Technology, Govt. of India, New Delhi. Authors are thankful to Antonella Peresan for critical comments, which have improved the quality of the manuscript greatly.

Supplementary material

531_2018_1603_MOESM1_ESM.docx (33 kb)
Supplementary material 1 (DOCX 32 KB)

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Authors and Affiliations

  • Prosanta Kumar Khan
    • 1
  • Jayashree Banerjee
    • 1
  • Sk Shamim
    • 1
  • Manoranjan Mohanty
    • 2
  1. 1.Department of Applied GeophysicsIndian Institute of Technology (ISM)DhanbadIndia
  2. 2.Department of Science and TechnologyTechnology Bhavan, Government of IndiaNew DelhiIndia

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