(Q57837320)

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The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum

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The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum (English)

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main subject

People's Republic of China

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1 reference

1 reference

3

Frank Lehmkuhl

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author name string

Xiaoping Yang

series ordinal

1

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Karl Tilman Rost

series ordinal

2

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Zhu Zhenda

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4

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John Dodson

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5

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publication date

January 2004

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published in

Quaternary International

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volume

118-119

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page(s)

69-85

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cites work

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

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Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years

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A 13,000-year climate record from western Tibet

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Paleoclimatic evolution of the Uvs Nuur basin and adjacent areas (Western Mongolia)

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

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Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (Western China and Western Mongolia)

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Geomorphological investigations and luminescence dating in the southern part of the Khangay and the Valley of the Gobi Lakes (Central Mongolia)

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Holocene--late pleistocene climatic ice core records from qinghai-tibetan plateau

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Late Quaternary palaeoenvironment change and landscape evolution along the Keriya River, Xinjiang, China: the relationship between high mountain glaciation and landscape evolution in foreland desert regions

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Variability of Monsoon Climate in East Asia at the End of the Last Glaciation

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Identifiers

DOI

10.1016/S1040-6182(03)00131-9

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ADS bibcode

2004QuInt.118...69Y

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(Q57837320)

The evolution of dry lands in northern China and in the Republic of Mongolia since the Last Glacial Maximum

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