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31 gru 2020 · The paper discusses the geomorphology of the Sunda Trench, an oceanic trench located in the eastern Indian Ocean along the Sumatra and Java Islands of the Indonesian archipelago.
Western Sundaland was a combination of basin opening and strike-slip transpressional deformation. The configuration suggests a free boundary particularly to the east (trench pull associated with the Proto-South China Sea subduction; JavaeSulawesi trench subduction rollback).
The study is focused on the Sunda Trench (also earlier called Java Trench), the deepest oceanic depression of the Indian Ocean, stretching 4–5 km parallel to the Sunda Island Arc, along its foot (Becker et al., 2009).
The western and southern borders of Sundaland are clearly marked by the deeper waters of the Sunda Trench – some of the deepest in the world – and the Indian Ocean. [4]
1 gru 2014 · Structural map of the major ridges and basins of South Sundaland from SE Borneo to Eastern Java and Flores basins. The region of East Java–Madura–Kanggean south of the Meratus Mountains and Bawean Arch (Figure 5, Figure 6), includes the Java basins and continental ridges (Ketapang High/North Madura ridge).
1 gru 2013 · Abstract. Most of the basins developed in the continental core of SE Asia (Sundaland) evolved since the Late Cretaceous in a manner that may be correlated to the conditions of the subduction in...
As shown in Fig. 2, the most significant tectonic feature is the Manila Trench, a 1100-km long seismic zone between South Taiwan and Mindoro Island, along which Sunda (SU) block is subducting ...
