Abstract:<p>The outer wedge of the Indo-Burma wedge (IBW) has resulted due to oblique subduction of the Indian Plate below the Burma. In this study, we will use the analysis of outcrop-scale structures from Tripura-Mizoram fold belt (TMFB) to evaluate the structural evolution of the outer wedge of IBW. TMFB belongs to the widest section of the outer wedge that stretches from east to west for around 270 km (along 23.5&#176; N latitude). The first order structure of the outer wedge is characterized … Show more
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