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Earth, Planets and Space
Fig. 4 | Earth, Planets and Space

Fig. 4

From: Seismic structures of the 154–160 Ma oceanic crust and uppermost mantle in the Northwest Pacific Basin

Fig. 4

Respective comparisons of observed record sections (top) and synthetic seismograms (bottom) for MTr6-79 (a: left) and for MTr8-15 (b: right). Calculated travel time curves for refraction arrivals from the crusts (P c ), from the uppermost mantle (P n ), and later phases through the crusts (P g ) are shown in the records together with reflection arrivals from the Moho (P m P).

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