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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Vydáno v:	Global and planetary change Ročník 229; s. 104224
Hlavní autoři:	Li, Baofeng, Feng, Qi, Wang, Xin, Li, Zaijun, Wang, Fei, Zhao, Chenguang, Yu, Tengfei, Chen, Weiyu
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Elsevier B.V 01.10.2023
Témata:	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
On-line přístup:	Získat plný text
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