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Fig. 2 | Earth, Planets and Space

Fig. 2

From: Dissimilar receiver functions observed at very close stations in the Kii Peninsula, central Japan: features and causes

Fig. 2

Estimated receiver functions. Receiver functions observed at N.WTRF (a, c) and N.WATH (b, d). Low-pass filters with f c  = 1.5 Hz (a, b) and 1.0 Hz (c, d) were applied. Horizontal and vertical axes represent delay time and backazimuth of teleseismic waveforms, respectively. Vertical green lines indicate the assumed arrival time of converted phases at the oceanic Moho discontinuity. The depth of Moho discontinuity (z) and plunge azimuth (ζ) reported by Shiomi and Park (2008) are shown on the right top of c and d

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