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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...
Slope Stability and Slope Formation in the Flysch Zone of the Vienna Forest (Austria)
Slope Stability Slope Formation Flysch Zone Vienna Forest Austria
2009/9/3
The Rhenodanubian Flysch of the northern Vienna Forest is composed of various layers of sandstones, marly shales, calcareous marls, and clay shists, which are covered by Quaternary periglacial cover b...
Through high-resolution research of sedimental chronology and the sediment environmental indexes, such as graininess, minerals, magnetic parameters, pigment content, organic carbon and chr...