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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Bibliographic Details
Main Author: Perpustakaan UGM, i-lib
Format: Article NonPeerReviewed
Published: [Yogyakarta] : Universitas Gadjah Mada 1998
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Online Access:https://repository.ugm.ac.id/18805/
http://i-lib.ugm.ac.id/jurnal/download.php?dataId=1612
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Institution: Universitas Gadjah Mada