摘要

To reconstruct a continuous record of paleowind patterns from eolian sequences, low field anisotropy of magnetic susceptibility (AMS) is considered to be a useful paleowind- retrieving proxy. This paper reports the AMS-based reconstruction of the paleowind direction variations spanning the past 1.4 Ma (million years) in the northeastern flank of the Qilian Mountains. Our results suggest that a NW-SE paleowind regime prevailed between 1.4 Ma and 0.78 Ma and a stable prevailing paleowind of NE-SW direction was established around 0.5 Ma after a period of transition (0.78 similar to 0.5 Ma). The ending time of the earlier paleowind pattern (0.78 Ma) seems to be approximately coincident with the reported ending time of the reconstructed major tectonic uplift event occurred in 1.2 similar to 0.8 Ma. This coincidence may imply that the near surface atmospheric circulation Pattern might have causally related with the Tibetan Plateau tectonic uplift.