Sediment provenances shift driven by sea level and Indian monsoon in the southern Bay of Bengal since the last glacial maximum

Sediment provenances shift driven by sea level and Indian monsoon in the southern Bay of Bengal since the last glacial maximum

The Tibetan Plateau uplift has induced the formation of the largest sediment source-sink system in the northeast Indian Ocean, which has become an ideal region for investigating land-sea interaction processes. However, many questions regarding sediment transport patterns and their controlling factor...

Disgrifiad llawn

Manylion Llyfryddiaeth
Prif Awduron: Shengfa Liu, Wenxing Ye, Hui Zhang, Peng Cao, Jingrui Li, Xingquan Sun, Xiaoyan Li, Xisheng Fang, Somkiat Khokiattiwong, Narumol Kornkanitnan, Xuefa Shi
Fformat: Erthygl
Iaith:English
Cyhoeddwyd: Frontiers Media S.A. 2023-01-01
Cyfres:Frontiers in Marine Science
Pynciau:
last glacial maximum (LGM)
sea level
Indian monsoon
dynamical process
Bay of Bengal (BoB)
sedimentary pattern
Mynediad Ar-lein:https://www.frontiersin.org/articles/10.3389/fmars.2023.1106663/full

Rhyngrwyd

https://www.frontiersin.org/articles/10.3389/fmars.2023.1106663/full

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