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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...
The eastern and western fronts of plate movement in Taiwan Island and Tibetan Plateau respectively are the two major sources of tectonic force for the morphogensis during Quaternary in Chi...
On the basis of extensive survey to the Quaternary paleosols, soils and weathering layers in the vast northern China and the Loess Plateau, we found some unusually special phenomena of che...