Formation of the upper reaches of the Yellow River: Provenance evidence from the strata of the Yellow River sedimentary basin

The age of the formation of the upper reaches of the Yellow River is controversial, ranging from the Pliocene to the Middle Pleistocene. However, determining the source of the detrital materials within the Yellow River sedimentary basins outside the Tibetan Plateau can provide important evidence for...

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Veröffentlicht in:	Global and planetary change Jg. 229; S. 104224
Hauptverfasser:	Li, Baofeng, Feng, Qi, Wang, Xin, Li, Zaijun, Wang, Fei, Zhao, Chenguang, Yu, Tengfei, Chen, Weiyu
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Elsevier B.V 01.10.2023
Schlagworte:	basins China climate change detritus drainage systems East Asian monsoon system evolution Geochemical fingerprint Heavy mineral assemblage monsoon season Pleistocene epoch Pliocene epoch provenance Sedimentary basin tectonics Upper reaches of the Yellow River Yellow River China Yellow River Sedimentary basin Upper reaches of the Yellow River Geochemical fingerprint Heavy mineral assemblage East Asian monsoon system
ISSN:	0921-8181, 1872-6364
Online-Zugang:	Volltext
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