Multiple volcanic episodes of the Kermanshah forearc basin, SW Iran: a record of the deactivation and re-initiation of Neotethyan subduction involving a mid-oceanic ridge

Supplementary Fig. S3 - Concordia diagrams of zircon U–Pb data for the pyroclastic samples from the low segment of the upper volcaniclastic succession (A, B, C, and E), for the gabbros (F, G, H, and I), and for the leucogranite (J, K, L, and M) that intruded into the upper volcaniclastic succession, for the gabbros intruded into serpentinite (N and O). (D) shows the histogram of 206Pb/238U ages of the zircons from the tuff sample (total 70 analyses).