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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| Format: | Thesis |
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[Yogyakarta] : Universitas Gadjah Mada
2013
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