Origin and provenance of the surficial sediments in the subenvironments of the East China Sea

DOU Yanguang; CHEN Xiaohui; LI Jun; CAI Feng; WEN Zhenhe; XU Gang; ZOU Liang

doi:10.16562/j.cnki.0256-1492.2018.04.002

Marine Geology & Quaternary Geology > 2018 > 38(4): 21-31. > DOI: 10.16562/j.cnki.0256-1492.2018.04.002

DOU Yanguang, CHEN Xiaohui, LI Jun, CAI Feng, WEN Zhenhe, XU Gang, ZOU Liang. Origin and provenance of the surficial sediments in the subenvironments of the East China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(4): 21-31. DOI: 10.16562/j.cnki.0256-1492.2018.04.002

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Origin and provenance of the surficial sediments in the subenvironments of the East China Sea

DOU Yanguang^1,2,,
CHEN Xiaohui^1,3,
LI Jun^1,3,
CAI Feng^1,3,
WEN Zhenhe^1,3,
XU Gang^1,2,
ZOU Liang^1,3

1.
Key Laboratory of Marine Hydrocarbon Resource of Environmental Geology, Ministry of Land and Resources, China Geology Survey, Qingdao Institute of Marine Geology, Qingdao 266071, China
2.
Laboratory for Marine Geology and Environment, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China
3.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China

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Received Date: January 29, 2018
Revised Date: May 03, 2018

Graphical Abstract

Abstract

Abstract

Grain size and clay mineral composition are analyzed for the surface sediments in various depositional units of the East China Sea including its outer shelf and slope, and the Okinawa Trough.Upon the basis, the origin and provenance of the sediments are discussed.Results show that the grain size of the sediments becomes finer gradually from the outer continental shelf, slope, to the Okinawa Trough.The sediments in the outer continental shelf are dominated by beach sands or breaker zone deposits formed during the deglacial transgression of late Pleistocene, and belong to the so-called "relict sediment", while the sediment on the western slope of the Okinawa Trough is characterized by gravity flow deposits, indicating a transportation pattern from the outer continental shelf to the Trough.Suspended deposits predominate the bottom fine sediment of the Okinawa Trough, having the characteristics of bathyal deposits.They are mainly from the rivers of Taiwan and Mainland China, such as the Changjiang and Minjiang Rivers.Provenance study reveals that the fine materials from Taiwan is mainly transported by Kuroshio Current, and the fine sediments from Mainland China are mainly transported by various transportation mechanisms, such as the"near-bottom lateral transportation"and"storage in winter and transporting in summer."
- depositional units,
- grain size,
- clay mineral,
- formation reason of surface sediment,
- sediment provenance,
- East China Sea

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References (52)

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Origin and provenance of the surficial sediments in the subenvironments of the East China Sea