Erosion, fault initiation and topographic growth of the North Qilian Shan (northern Tibetan Plateau)

New apatite (U-Th)/He from the northeastern
\nmargin of the Tibetan Plateau (north
\nQilian Shan) indicate rapid cooling began at
\n~10 Ma, which is attributed to the onset of
\nfaulting and topographic growth. Preservation
\nof the paleo-PRZ in the hanging wall and
\ngrowth ... View More