Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years

[1]  S. Clemens,et al.  Comments on “Paleoclimatic Significance of the Mineral Magnetic Record of the Chinese Loess and Paleosols” , 1992, Quaternary Research.

[2]  J. Beer,et al.  10Be in Chinese loess , 1992 .

[3]  S. Forman.  Late Pleistocene chronology of loess deposition near Luochuan, China , 1991, Quaternary Research.

[4]  J. T. Wang,et al.  Partly pedogenic origin of magnetic variations in Chinese loess , 1990, Nature.

[5]  R. Fairbanks.  A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation , 1989, Nature.

[6]  N. Pisias,et al.  A direct link between the China loess and marine δ18O records: aeolian flux to the north Pacific , 1989, Nature.

[7]  B. Maher,et al.  Formation of ultrafine-grained magnetite in soils , 1988, Nature.

[8]  G. Kukla,et al.  Pleistocene climates in China dated by magnetic susceptibility , 1988 .

[9]  J. Kutzbach,et al.  Monsoon variability over the past 150,000 years , 1987 .

[10]  L. Yan-chou,et al.  Thermoluminescence dating of the Malan loess at Zhaitang, China , 1987 .

[11]  F. Heller,et al.  Palaeoclimatic and sedimentary history from magnetic susceptibility of loess in China , 1986 .

[12]  J. Kutzbach,et al.  The Influence of Changing Orbital Parameters and Surface Boundary Conditions on Climate Simulations for the Past 18 000 Years , 1986 .

[13]  J. Mélice,et al.  Magnetic susceptibility record of Chinese Loess , 1990, Transactions of the Royal Society of Edinburgh: Earth Sciences.

[14]  P. Townsend,et al.  Thermoluminescence dating of a 10 m loess profile in Pakistan , 1988 .

[15]  G. Kukla.  Loess stratigraphy in central China , 1987 .

[16]  Dongsheng Liu,et al.  Loess and the environment , 1985 .

[17]  Yongyan Wang,et al.  The Recent research of loess in China : stratigraphy, magnetostratigraphy, chronology, pedology, paleontology and paleoclimatology , 1984 .

[18]  Z. An.  A CLIMATOSTRATIGRAPHIC SUBDIVISION OF LATE PLEISTOCENE STRATA NAMED BY MALAN FORMATION IN NORTH CHINA , 1984 .