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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Main Authors: | , Rian Amukti, , Dr. rer. nat. Wiwit Suryanto, M.Si |
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Format: | Theses and Dissertations NonPeerReviewed |
Published: |
[Yogyakarta] : Universitas Gadjah Mada
2013
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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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