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Damming of River Indus during Late Quaternary in Ladakh Region of Trans-Himalaya, NW India：Implications to Lake formation-climate and tectonics
Late Quaternary Holocene Trans Himalaya Indus Palaeolake deposits climate
2014/1/16
Indus river valley basin in Northwest Indian Himalaya is tectonically unstable, exhibiting a complex topography, landscape relief and varied Quaternary sedimentation. A 422 km transact along the Indus...