PEMODELAN KERAK DAN BAGIAN ATAS MANTEL BUMI DI BAWAH PULAU JAWA BAGIAN TENGAH MENGGUNAKAN DATA RECEIVER FUNCTION

Receiver function analysis has been done to prove a low velocity anomaly between Merapi volcano and mount Lawu (Merapi Lawu Anomaly) at depth 5-15 km. This method has advantage in modeling the subsurface structure from a three components seismometer. Data were rotated from ZNE component to ZRT compo...

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Bibliographic Details
Main Authors: , Rian Amukti, , 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/123217/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=63328
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Institution: Universitas Gadjah Mada
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