VARIASI KEDALAMAN DISKONTINUITAS MOHO DI JAWA TENGAH DAN YOGYAKARTA BERDASARKAN DATA RECEIVER FUNCTION
Mohorovi�i� discontinuity or Moho is a boundary between the crust and upper mantle. This boundary has a characteristic that P wave velocity increased from 6,75 km/s up to 8 km/s. The velocity contrast between crust and mantle can be used to estimate the crustal thickness. Tectonic process is a fac...
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| Main Authors: | , |
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| Format: | Theses and Dissertations NonPeerReviewed |
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[Yogyakarta] : Universitas Gadjah Mada
2013
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| Online Access: | https://repository.ugm.ac.id/123790/ http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=63905 |
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| Institution: | Universitas Gadjah Mada |
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