The late Miocene and Pliocene climate in East Asia as recorded by grain size and magnetic susceptibility of the Red Clay deposits (Chinese Loess Plateau)
- 25 February 2004
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 204 (3-4) , 239-255
- https://doi.org/10.1016/s0031-0182(03)00729-6
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Holocene loess accumulation and soil development at the western edge of the Chinese Loess Plateau: implications for magnetic proxies of palaeorainfallPublished by Elsevier ,2002
- Aeolian origin and palaeoclimatic implications of the ?red clay? (north China) as evidenced by grain-size distributionJournal of Quaternary Science, 2001
- Pedostratigraphy and paleomagnetism of a ∼7.0 Ma eolian loess–red clay sequence at Lingtai, Loess Plateau, north-central China and the implications for paleomonsoon evolutionPublished by Elsevier ,1999
- East Asia winter monsoon variations on a millennial time-scale before the last glacial-interglacial cycleJournal of Quaternary Science, 1999
- Loess chronology of the Middle and Upper Pleistocene in TadjikistanInternational Journal of Earth Sciences, 1998
- Evaluation of the Plio‐Pleistocene astronomical timescalePaleoceanography and Paleoclimatology, 1996
- Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and CenozoicJournal of Geophysical Research, 1995
- The paleoclimatic record provided by eolian deposition in the deep sea: The geologic history of windReviews of Geophysics, 1994
- Sensitivity of Eurasian Climate to Surface Uplift of the Tibetan PlateauThe Journal of Geology, 1993
- Late quaternary dust flow on the chinese Loess PlateauCATENA, 1991