Sediment provenance in the Northern South China Sea since the Late Miocene

The timing of the onset of Taiwan sediment input to the northern South China Sea (SCS) is still controversial even though many provenance proxies had been used. To analyze the change of Taiwan input since the Late Miocene (11.63–0 Ma), we applied the major-element-based proxies R AK a...

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Bibliografiska uppgifter

Huvudupphov:	Hu Zhe, Huang Baoqi, Geng Li, Wang Na
Materialtyp:	Artigo
Språk:	Inglês
Utgiven:	De Gruyter 2022-12-01
Serie:	Open Geosciences
Ämnen:	south china sea source-to-sink late miocene taiwan input sea level
Länkar:	https://doi.org/10.1515/geo-2022-0454
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