Block-diagram showing a cross-section of the subduction zone beneath the Philippines. The Philippine tectonic plate (on the right) dives under the Eurasian plate (on the left).

Block-diagram showing a cross-section of the subduction zone beneath the islands of Java, Bali, Lombok and Sumbawa in Indonesia.

Block-diagram showing a cross-section of the Sunda Megathrust. The Indo-Australian tectonic plate (on the left) dives under the Eurasian plate (on the right).

Block-diagram showing a cross-section of the subduction zone beneath the Philippines. The Philippine tectonic plate (on the right) dives under the Eurasian plate (on the left).

Block-diagram showing a cross-section of the subduction zone beneath the islands of Java, Bali, Lombok and Sumbawa in Indonesia.

Block-diagram showing a cross-section of the Sunda Megathrust. The Indo-Australian tectonic plate (on the left) dives under the Eurasian plate (on the right).

Left hand side: Inversion results for n = 1, Q = 170, f = 10 Hz and b = 1 km s−1 .

Owing to recent advances in observational methods and modeling techniques, the development of physical models of the seismic cycle with predictive power may seem at reach in a foreseeabl

eosmedia@ntu.edu.sg
Shireen FEDERICO
Tel: (65) 6908-2265