Figure 2
From: Mantle wedge diapirs detected by a dense seismic array in Northern Taiwan

Locations of Formosa Array (the upper panel) and strong later P-waves (P2) are recorded at the vertical seismograms generated by 4 earthquakes (Events A, B, C and D shown at the lower panels) from the subduction zone beneath northern Taiwan. This figure was created by Generic Mapping Tools (GMT version 4.5.2; URL: gmt.soest.hawaii.edu) and SAC software (version 101.5; URL: ds.iris.edu).