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• W1956067952 endingPage "3052" @default.
• W1956067952 startingPage "3034" @default.
• W1956067952 abstract "Abstract The East China Sea is characterized by wide continental shelf receiving a huge input of terrigenous matter from both large rivers and mountainous rivers, which makes it an ideal natural laboratory for studying sediment source‐to‐sink transport processes. This paper presents mineralogical and geochemical data of the clays and bulk sediments from the rivers entering the East China Sea, aiming to investigate the general driving mechanism of silicate weathering and sediment transport processes in East Asian continental margin. Two types of river systems, tectonically stable continental rivers and tectonically active mountainous rivers, coexist in East Asia. As the direct weathering products, clays can better reflect the silicate weathering regimes within the two river systems. Provenance rock types are not the dominant factor causing silicate weathering intensity difference existed in the East Asian rivers. The silicate weathering intensity of tectonically stable river basins is primarily driven by monsoon climate, and the sediment transfer is relatively slow because of natural trapping process and increasing damming effect. The geochemistry of these river‐borne sediments can thus indicate paleo‐weathering intensities in East Asian continent. In contrast, silicate weathering intensity in tectonically active mountainous rivers is greatly limited by strong physical erosion despite the high temperature and highest monsoon rainfall. The factors controlling silicate weathering in tectonically active catchments are complex and thus, it should be prudent to use river sediment records to decipher paleoclimate change. These two different silicate weathering regimes and sediment transport processes are manifestations of the landscape evolution and overall dominate the sedimentation in Asian continental margin." @default.
• W1956067952 created "2016-06-24" @default.
• W1956067952 creator A5003753200 @default.
• W1956067952 creator A5033178355 @default.
• W1956067952 creator A5037808701 @default.
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• W1956067952 creator A5063131315 @default.
• W1956067952 creator A5069273263 @default.
• W1956067952 creator A5075789051 @default.
• W1956067952 date "2015-09-01" @default.
• W1956067952 modified "2023-10-14" @default.
• W1956067952 title "Geochemistry of river-borne clays entering the East China Sea indicates two contrasting types of weathering and sediment transport processes" @default.
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