Low δ18O mantle derived magma in Panjal Traps overprinted
by SIMS zircon analysis Pakistan Fig. 1. Group I eclogites are medium to coarse grained, composed of porphyroblasts, omphacite, amphibole, and symplectites replac ing and omphacite with abundant rutile, titanite, and ilmenite. Zircons are abundant and relatively large ~500 μm. Pressure temper ature conditions of 2.2 ± 0.3 GPa and 704 ± 92 °C were





































