Neogene stress pattern evolution along the semangko fault, sumatra
ABSTRACT Western Indonesia corresponds to the subduction of the Indo-Australian plate beneath the Eurasian plate. The convergence between the two plates is oblique along the Sumatra trench. The1650-km-long, dextral Great Sumatran fault has been considered to accommodate the lateral component of conv...
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[Yogyakarta] : Universitas Gadjah Mada
1998
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