Subduction zone beneath Sumatra, 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).

Cross sections were organized in increasing depth. Site 4. Slopes of the hogbacks studied ranged from 0.07 to 0.27, whereas slopes of the scarps ranged from 0.19 to 0.66 (Table 1, Fig. 7a). A weak positive correlation exists between distance from the trench and a slope of the scarps – the seismic expression areas (Fig. 7b).

May 1, 2009 · The findings of this study indicate that the back-arc basins of Sumatra experienced severe extensional deformation during the Tertiary Period through a large pull-apart and slab rollback...

In this study, we overcome all these limitations by developing a probabilistic framework that combines imbalance handling and ensemble machine learning for landslide susceptibility mapping.

Question: B. Sumatra Make the Sumatra cross-section visible and show the Elevation Profile. 9. On the cross section below, mark the boundary between the Indo-Australian and Eurasian plates at the Earth's surface with an X. Mark the location of volcanoes with a star.

Part B: Convergent Plate Boundary (Sumatra) Uncheck all the other features and now make the Sumatra cross-section visible and Show the Elevation Profile. It should look somewhat like this one: Questions/ Tasks B1.

Make the Sumatra cross-section visible and Show the Elevation Profile. On the cross - section below, which letters represent the boundary between the Indo - Australian and Eurasian plates and the volcanoes' location.

Geological cross section field in South Sumatra Basin represent the configuration of the reservoir and sealing rock. ... the basin where it is draped over basement highs and has been proven...