Sedimentary facies and material source of core DGKS9617 in the east China sea

Hua Yu; Zhenxia Liu; Yingqian Xiong; Yoshiki Saito; Kunshan Wang

doi:10.4028/0-87849-958-x.410

Sedimentary facies and material source of core DGKS9617 in the east China sea

Hua Yu^*, Zhenxia Liu, Yingqian Xiong, Yoshiki Saito, Kunshan Wang

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

Abstract

A piston core DGKS9617, recovered from the northern part of the inner shelf of the East China Sea (ECS) is divided into two sedimentary facies: a tidal shallow marine facies (55-850 cm) and a shallow marine facies (0-55 cm). Although the sedimentary environments of its upper and lower parts are different, the provenance of the whole core does not change. The heavy mineral assemblage, the results of the discrimination function of Fe, Mn, V, Cr, Ni, Cu and Zn, the carbonate content and the Ba-Sr-Zn ternary diagram consistently show that the heavy mineral and geochemical characteristics of core DGKS9617 are similar to that of the Yangtze River sediments and that its sediment is mainly provided by the Yangtze River.

Original language	English (US)
Pages (from-to)	410-417
Number of pages	8
Journal	Key Engineering Materials
Volume	277-279
Issue number	I
DOIs	https://doi.org/10.4028/0-87849-958-x.410
State	Published - 2005
Externally published	Yes

Keywords

East China Sea
Elementary geochemistry
Heavy mineral
Material source

ASJC Scopus subject areas

General Materials Science
Mechanics of Materials
Mechanical Engineering

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

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10.4028/0-87849-958-x.410

Cite this

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title = "Sedimentary facies and material source of core DGKS9617 in the east China sea",

abstract = "A piston core DGKS9617, recovered from the northern part of the inner shelf of the East China Sea (ECS) is divided into two sedimentary facies: a tidal shallow marine facies (55-850 cm) and a shallow marine facies (0-55 cm). Although the sedimentary environments of its upper and lower parts are different, the provenance of the whole core does not change. The heavy mineral assemblage, the results of the discrimination function of Fe, Mn, V, Cr, Ni, Cu and Zn, the carbonate content and the Ba-Sr-Zn ternary diagram consistently show that the heavy mineral and geochemical characteristics of core DGKS9617 are similar to that of the Yangtze River sediments and that its sediment is mainly provided by the Yangtze River.",

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author = "Hua Yu and Zhenxia Liu and Yingqian Xiong and Yoshiki Saito and Kunshan Wang",

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doi = "10.4028/0-87849-958-x.410",

language = "English (US)",

volume = "277-279",

pages = "410--417",

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TY - JOUR

T1 - Sedimentary facies and material source of core DGKS9617 in the east China sea

AU - Yu, Hua

AU - Liu, Zhenxia

AU - Xiong, Yingqian

AU - Saito, Yoshiki

AU - Wang, Kunshan

PY - 2005

Y1 - 2005

N2 - A piston core DGKS9617, recovered from the northern part of the inner shelf of the East China Sea (ECS) is divided into two sedimentary facies: a tidal shallow marine facies (55-850 cm) and a shallow marine facies (0-55 cm). Although the sedimentary environments of its upper and lower parts are different, the provenance of the whole core does not change. The heavy mineral assemblage, the results of the discrimination function of Fe, Mn, V, Cr, Ni, Cu and Zn, the carbonate content and the Ba-Sr-Zn ternary diagram consistently show that the heavy mineral and geochemical characteristics of core DGKS9617 are similar to that of the Yangtze River sediments and that its sediment is mainly provided by the Yangtze River.

AB - A piston core DGKS9617, recovered from the northern part of the inner shelf of the East China Sea (ECS) is divided into two sedimentary facies: a tidal shallow marine facies (55-850 cm) and a shallow marine facies (0-55 cm). Although the sedimentary environments of its upper and lower parts are different, the provenance of the whole core does not change. The heavy mineral assemblage, the results of the discrimination function of Fe, Mn, V, Cr, Ni, Cu and Zn, the carbonate content and the Ba-Sr-Zn ternary diagram consistently show that the heavy mineral and geochemical characteristics of core DGKS9617 are similar to that of the Yangtze River sediments and that its sediment is mainly provided by the Yangtze River.

KW - East China Sea

KW - Elementary geochemistry

KW - Heavy mineral

KW - Material source

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DO - 10.4028/0-87849-958-x.410

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SN - 1013-9826

VL - 277-279

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JF - Key Engineering Materials

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ER -

Sedimentary facies and material source of core DGKS9617 in the east China sea

Abstract

Keywords

ASJC Scopus subject areas

UN SDGs

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