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- W2362892605 abstract "The ancient Pearl River delta in the early Eocene shelf of Pearl River Mouth Basin is defined as setting source,the canyon channels in the slope as paths,and the deep-water fan in the slope as sink.They form a sedimentary system from source to sink.The sedimentary system can be divided into shelf subsystem and slope subsystem.The relative variation to sea level,regional structural movement and source supply strength controlled the development and evolution of the sedimentary system.In third-order sequence framework,the delta in the shelf subsystem developed into a shelf-edge delta in the LST,and the delta front crossed over shelf break to connect with the canyon channels in the slope subsystem.The transporting mechanism of clastic material is changed:from the traction current controlled by river,wave and tide to the gravity current controlled by gravity and physiognomy.Baiyun deep-water fan sink of the slope subsystem is formed in the upper slope,and the sedimentary development mode of two bodies-one connection path is formed.In TST and HST phases the delta devoloped to be shelf delta,the delta front can not cross over the break and deposits again.In the slope subsystem,marine mud deposits because of no outer source supply,so the sedimentary development mode of one body-one connection path is formed.During the evolution process of whole sedimentary system,clastic material transports between the subsystems under different time-space matching relationships,which makes the shelf subsystem connect with the slope subsystem.So the whole sedimentary system is an episodic sedimentary mode." @default.
- W2362892605 created "2016-06-24" @default.
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- W2362892605 date "2011-01-01" @default.
- W2362892605 modified "2023-09-22" @default.
- W2362892605 title "Composition and reservoir body distribution of continental shelf-continental slope sedimentary system in early Eocene in Pearl River Mouth Basin" @default.
- W2362892605 hasPublicationYear "2011" @default.
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