The shear wave velocity structure of the crust and uppermost mantle beneath Tagaytay, Philippines inferred from receiver function analysis

Depths of the partially melted zone and the Moho discontinuity are probably at 18 kilometers and 34 kilometers, respectively beneath Tagaytay seismic station, Luzon, Philippines. This conclusion is based on the shear‐wave velocity structure determined in this study, which indicates the presence of a...

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Veröffentlicht in:	Geophysical research letters 1995-12, Vol.22 (23), p.3143-3146
Hauptverfasser:	Besana, G. M., Shibutani, T., Hirano, N., Ando, M., Bautista, B., Narag, I., Punongbayan, R. S.
Format:	Artikel
Sprache:	eng
Schlagworte:	Earth sciences Earth, ocean, space Earthquakes Earthquakes, seismology Exact sciences and technology Internal geophysics Moho discontinuity Philippines Receivers Seismic phenomena Solid-earth geophysics, tectonophysics, gravimetry Sound waves Stations Waveforms
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