Sea level induced variations in clay mineral composition in the southwestern South China Sea over the past 17,000 yr

Variations in clay mineral composition of sediment cores from the margin and continental slope of the Sunda Shelf (southern South China Sea, SE Asia) covering the past 17,000 yr reflect changing influences of sediment sources together with clay mineral partitioning processes in shallow waters. We id...

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Veröffentlicht in:	Marine geology 2008-05, Vol.250 (3), p.199-210
Hauptverfasser:	Steinke, Stephan, Hanebuth, Till J.J., Vogt, Christoph, Stattegger, Karl
Format:	Artikel
Sprache:	eng
Schlagworte:	clay minerals last deglaciation Marine sea level changes South China Sea Sunda Shelf
Online-Zugang:	Volltext
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