The authors obtained a 671 m long loess core through drilling on the northern slope of the West Kunlun Mountains. In this paper, the authors investigated its 207 m long loess core by integrating both rockmagnetic and grain size proxies. The study results suggest that the low coercivity minerals,i.e,magnetite and maghemite are dominated in the loess. The characteristics of typical hysteresis loops probably imply the presence of paramagnetic component to a certain extent. These results improved the understanding of the enhancing mechanism of susceptibility at different sites with different paleoenvironmental conditions: in comparison with the ultrafine pedogenic minerals,coarse lithogenic magnetic minerals can also play an important role in enhancement of MS at some time.