Tectonics of the Indonesian Region_Warren Halminton
The continuous, curving Andaman-Sumatra-Java-Timor-outer Banda-Seram subduction system now bounds the Indonesian region against the Indian OceanAustralian plate. The Benioff zone of mantle earthquakes dipping under Indonesia from the trench has gentle dips at shallow depths but steepens downward in most sectors (fig. 1).