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The subduction of the Indian-Australian Plate beneath the Eurasian Plate is oblique (~45o) along Sumatra.A major zone of dextral strike slip displacement along Sumatra Island, called the Sumatra Fault, partially accommodates the oblique convergence off Sumatra. On the contrary, the subduction is nor...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/14568 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
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