T. S. Liu

发表

Stacked 2.6‐Ma grain size record from the Chinese loess based on five sections and correlation with the deep‐sea δ18O record

S. L. Yang, Z. Ding, E. Derbyshire, 2002 .

Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China

Shuzhen Peng, W. Ruddiman, Q. Hao, 2002, Nature.

Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution

Jimin Sun, Z. Ding, E. Derbyshire, 2005 .

Response of climate to solar forcing recorded in a 6000-yearδ18O time-series of Chinese peat cellulose

X. Qin, Tung-sheng Liu, J. Beer, 2000 .

Grain size variation in two lakes from margin of Asian Summer Monsoon and its paleoclimate implications

Weijian Zhou, Hong Wang, Jie Zhou, 2021 .

High resolution climate record from the Beijing area during the Last Glacial‐Interglacial Cycle

J. Bloemendal, P. Hesse, X. M. Liu, 1998 .

Initial intensification of East Asian winter monsoon at about 2.75 Ma as seen in the Chinese eolian loess‐red clay deposit

S. L. Yang, Z. Ding, S. Xiong, 2003 .

Preliminary magnetostratigraphy of a thick eolian red clay‐loess sequence at Lingtai, the Chinese Loess Plateau

S. L. Yang, Z. Ding, Tung-sheng Liu, 1998 .

Coeval changes in grain size and sedimentation rate of eolian loess, the Chinese Loess Plateau

S. L. Yang, T. S. Liu, Z. Yu, 2001 .

Damped fluctuations in Chinese loess grain size

S. L. Yang, Z. Ding, S. Xiong, 2003 .

Northwestward decline of magnetic susceptibility for the red clay deposit in the Chinese Loess Plateau

S. L. Yang, Z. Ding, S. Xiong, 2002 .