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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Bibliographic Details
Main Authors: , NOOR ACHID YUNARTHA, , Dr. rer. nat. Wiwit Suryanto, M.Si
Format: Theses and Dissertations NonPeerReviewed
Published: [Yogyakarta] : Universitas Gadjah Mada 2013
Subjects:
ETD
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