A critical review of field relationships and gravitational origin of active normal faults in the Kashmir basin, NW Himalaya
Kashmir basin is a piggyback basin that has developed at the last stage of the ongoing collision between India and Eurasia, and it is ~4 Ma old and contains 1300 m thick blanket of Plio-Pleistocene to Holocene deposits. These unconsolidated sediments are locally known as Karewas, which are deformed...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Elsevier
2020-12-01
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| Series: | Journal of Asian Earth Sciences: X |
| Subjects: | |
| Online Access: | http://www.sciencedirect.com/science/article/pii/S2590056020300189 |