Fig. 13From: Tectonic significance of Triassic mafic rocks in the June Complex, Sanandaj–Sirjan zone, Iran a Tectonic model of the emplacement of the mafic rocks in the June Complex. The model is largely modified after Saccani et al. (2013a), who assumed no plume-MORB interaction in the northeastern/northern side of the Neotethyan Ocean. b Detail of the suggested emplacement of basalts in the June Complex rising up through the Sanandaj–Sirjan crustBack to article page