Six million years of magnetic grain-size records reveal that temperature and precipitation were decoupled on the Chinese Loess Plateau during ~ 4.5–2.6 Ma

Tibet forcing of mid-Pleistocene synchronous enhancement of East Asian winter and summer monsoons revealed by Chinese loess record

(2012) Wenxia Han et al.   QUATERNARY RESEARCH

Paleomonsoon route reconstruction along a W–E transect in the Chinese Loess Plateau using the anisotropy of magnetic susceptibility: Summer monsoon model

(2010) Rui Zhang et al.   EARTH AND PLANETARY SCIENCE LETTERS

Climatic interpretation of a 1.9 Ma environmental magnetic record of loess deposition and soil formation in the central eastern Pampas of Buenos Aires, Argentina

(2010) Clifford W. Heil Jr. et al.   QUATERNARY SCIENCE REVIEWS

Consistent grain size distribution of pedogenic maghemite of surface soils and Miocene loessic soils on the Chinese Loess Plateau

(2009) Junsheng Nie et al.   JOURNAL OF QUATERNARY SCIENCE

Tibetan uplift intensified the 400 k.y. signal in paleoclimate records at 4 Ma

(2008) J. Nie et al.   GEOLOGICAL SOCIETY OF AMERICA BULLETIN

Particle size separation and evidence for pedogenesis in samples from the Chinese Loess Plateau spanning the past 22 m.y

(2008) Qingzhen Hao et al.   GEOLOGY