Seismology: Earthquake risk on the Sunda trench

@article{Nalbant2005SeismologyER,
  title={Seismology: Earthquake risk on the Sunda trench},
  author={Suleyman S. Nalbant and Sandy Steacy and Kerry Sieh and Danny Hilman Natawidjaja and John McCloskey},
  journal={Nature},
  year={2005},
  volume={435},
  pages={756-757}
}
On 28 March 2005 the Sunda megathrust in Indonesia ruptured again, producing another great earthquake three months after the previous one. The rupture was contiguous with that of the December 2004 Sumatra–Andaman earthquake, and is likely to have been sparked by local stress, although the triggering stresses at its hypocentre were very small — of the order of just 0.1 bar. Calculations show that stresses imposed by the second rupture have brought closer to failure the megathrust immediately to… Expand
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References

SHOWING 1-8 OF 8 REFERENCES
Indonesian earthquake: Earthquake risk from co-seismic stress
TLDR
This work has calculated the distributions of co-seismic stress on the contiguous Sunda trench subduction zone, as well as on the neighbouring, vertical strike–slip Sumatra fault, and finds an increase in stress on both structures that significantly boosts the already considerable earthquake hazard posed by them. Expand
Progressive failure on the North Anatolian fault since 1939 by earthquake stress triggering
SUMMARY 10 M ≥ 6.7 earthquakes ruptured 1000 km of the North Anatolian fault (Turkey) during 1939–1992, providing an unsurpassed opportunity to study how one large shock sets up the next. We useExpand
Seismic history and seismotectonics of the Sunda Arc
Historic records of the last 300 years reveal two great interplate earthquakes (1833, MW = 8¾ 1861, MW = 8¼–8½), which ruptured major segments of the Sumatra fore arc in western Indonesia; aExpand
Viscosity of oceanic asthenosphere inferred from remote triggering of earthquakes
TLDR
The postseismic stress evolution across the northern Pacific and Arctic basins is consistent with triggering of oceanic intraplate earthquakes, temporal patterns in seismicity at remote plate boundaries, and space-based geodetic measurements of anomalous velocity over an area 7000 by 7000 kilometers square during the 30-year period after the sequence. Expand
A Comparative Study of the Sumatran Subduction-Zone Earthquakes of 1935 and 1984
A M_s 7.7 earthquake struck the western, equatorial coast of Sumatra in December 1935. It was the largest event in the region since the two devastating giant earthquakes of 1833 and 1861. HistoricalExpand
The 1995 Kobe, Japan, earthquake: A long-delayed aftershock of the offshore 1944 Tonankai and 1946 Nankaido earthquakes
The 1995 Kobe earthquake produced predominantly right-lateral slip along the northeast-southwest-trending Nojima fault approximately 200 km landward of the Nankai trough, southwest Japan. The lastExpand
Paleogeodetic records of seismic and aseismic subduction from central Sumatran microatolls, Indonesia
We utilize coral microatolls in western Sumatra to document vertical deformation associated with subduction. Microatolls are very sensitive to fluctuations in sea level and thus act as natural tideExpand
List of Table Table 1 Hypocentral stresses in the Sumatran earthquake
  • Science 280,
  • 1998