Holocene climate change inferred from stratigraphy and OSL chronology of aeolian sediments in the Qaidam Basin, northeastern Qinghai–Tibetan Plateau

Paleoclimatic reconstruction based on aeolian sediments in the eastern Qaidam Basin (QB) has been hindered by the limited chronological data. Here we present 61 Optically Stimulated Luminescence (OSL) ages. On the basis of these OSL ages and the lithologic stratigraphy, we propose the ‘effective moi...

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Veröffentlicht in:	Quaternary research 2014-05, Vol.81 (3), p.488-499
Hauptverfasser:	Yu, LuPeng, Lai, ZhongPing
Format:	Artikel
Sprache:	eng
Schlagworte:	Aeolian activity Age Asian summer monsoon Basins Electromagnetic interference Holocene climate change Moisture OSL dating Qaidam Basin Qinghai–Tibetan Plateau Sand Sediments Stratigraphy Summer
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