Contemporary deformation study along Cambay and Narmada paleo-rift system, western part of Indian plate
The western part of the Indian plate, which includes three major paleo-rifts, the Kachchh, Narmada and Cambay basins, is tectonically active and has seen moderate to large earthquakes. Regional stress due to the convergence of the Indo-European plates is the main cause of deformation accumulation in...
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| Format: | Article |
| Language: | English |
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Elsevier
2024-01-01
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| Series: | Quaternary Science Advances |
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| Online Access: | http://www.sciencedirect.com/science/article/pii/S2666033424000042 |