Fluvial response to climate change during and after the Last Glacial Maximum in Central Anatolia, Turkey

Fluvial response to climate change during and after the Last Glacial Maximum (LGM) included incision–aggradation phases, recorded in sediment cores from the valley floor of the Kızılırmak in Central Anatolia. A numerical chronology was established by AMS dating of fluvial sediments and Ar–Ar dating...

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Veröffentlicht in:	Quaternary international 2010-08, Vol.222 (1), p.221-229
1. Verfasser:	Dooan, Uour
Format:	Artikel
Sprache:	eng
Schlagworte:	Freshwater
Online-Zugang:	Volltext
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