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This study presents a detailed analysis of the deformation in the western Deccan region of India, challenging the prevailing view of E–W extension related to India–Seychelles rifting. The authors propose that the deformation is characterized by N–S and NE–SW trending shear zones, indicating an oblique rifted margin rather than a simple E–W extension. The findings suggest that the rifting and volcanism were likely coeval, with significant implications for understanding the tectonics of the region.

Author

nawazsiddiqui100

Language

EN