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Depositional Elements and Settings of HD133 and HD77 Cores in the Taiwan Canyon
详细信息   
摘要
Located within and outside the Taiwan Strait in the northeastern South China Sea,with the water depths of 3 280 m and 3 378 m separately, two sediment cores HD133 and HD77 are carefully investigated through analysis of grain size,paleontology and calcium carbonate content.The controlling factors for the deep-water sands within these two sediment cores are as the following: temporally,terrigenous sediments are directly delivered into the deep-water settings,forming sand-rich deposits layer 2;spatially,submarine canyons are the conduits for terrigenous gravity flow,making the deposition occur firstly within the canyon.Thus,HD133 is richer in sand than HD77.

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