Figure 4 | Scientific Reports

Figure 4

From: Geoelectric characterisation of the junction of seismically active Delhi Hardwar Ridge and Delhi Sargodha Ridge

Figure 4

The schematic diagram (a) showing the formation of Aravallis during the Proterozoic due to the collision of Marwar Cratons and Bundelkhand Cratons, (b) the bulging in the forefront due to the collision of Indian and Eurasian plates during Eocene to Pliocene and (c) the N-S geological section of the Himalaya(after Irfan et al.16) showing the major thrusts (KKT: Karakoram Thrust; MCT: Main Central Thrust; MBT Main Boundary Thrust and HFT: Himalayan Frontal Thrust), suture zone (ITSZ: Indo Tsangpo Suture Zone) and formation of the bulge during Eocene to Pliocene.

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