Southeast (SE) Asia and its surrounding regions exhibit very complex structure and tectonics, where the Sunda Plate, Eurasian Plate, Philippine Sea Plate, Indian Plate, Australian Plate, and several small plates interact with each other (Figure 1). The Sunda Plate located in the center of the region constitutes land areas such as the Indochina Peninsula, Malay Peninsula, Indonesian islands (Sumatra, Java, Borneo, etc.), the Philippines, and broad oceanic areas such as the Sunda Shelf, the South China Sea (SCS), the Sulu Sea, and the Celebes Sea. The Sunda Plate is surrounded by well-developed subduction zones. Trenches of particular note are the Sunda Trench where the Indian Plate and the Australian Plate are subducting beneath the Sunda Plate from the west and the south, respectively, the Philippine Trench where the Philippine Sea Plate subducts beneath the Sunda Plate from the east, and the Manila Trench where the Sunda Plate subducts beneath the Philippine Sea Plate from the west. Seismic activity in this region is extremely high, and many large earthquakes have occurred at depths <100 km along the Sunda Trench and the Philippine Trench (Figure S1 in Supporting Information S1). In particular, the 2004 Sumatra-Andaman earthquake (Mw 9.1) that occurred on 26 December 2004 caused 230,000 deaths due to the strong ground motion and tsunami (Synolakis et al., 2005). Deep-focus earthquakes also occurred actively, and the 17 June 1996 earthquake off Maumere, Indonesia, recorded Mw 7.9 despite its focal depth of 587 km. Activity of arc volcanoes making up the volcanic front is also high in this region. For example, the Tambora volcano on Sumbawa Island, east of Java, caused the world's largest volcanic eruption in the recorded history on