中全新世以来琼东南陆架粘土矿物特征及物质来源

田旭; 徐方建; 吴淑壮; 张晋; 郭晨; 董江

doi:10.3799/dqkx.2015.134

Volume 40 Issue 9

Sep. 2015

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Article Navigation > Earth Science > 2015 > 40(9): 1497-1504

Tian Xu, Xu Fangjian, Wu Shuzhuang, Zhang Jin, Guo Chen, Dong Jiang, 2015. Clay Mineral Characteristics and Provenance of Continental Shelf Sediments in Eastern Hainan Island since Middle Holocene. Earth Science, 40(9): 1497-1504. doi: 10.3799/dqkx.2015.134

Citation:

Tian Xu, Xu Fangjian, Wu Shuzhuang, Zhang Jin, Guo Chen, Dong Jiang, 2015. Clay Mineral Characteristics and Provenance of Continental Shelf Sediments in Eastern Hainan Island since Middle Holocene. Earth Science, 40(9): 1497-1504. doi: 10.3799/dqkx.2015.134

Citation:

Tian Xu, Xu Fangjian, Wu Shuzhuang, Zhang Jin, Guo Chen, Dong Jiang, 2015. Clay Mineral Characteristics and Provenance of Continental Shelf Sediments in Eastern Hainan Island since Middle Holocene. Earth Science, 40(9): 1497-1504. doi: 10.3799/dqkx.2015.134

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Clay Mineral Characteristics and Provenance of Continental Shelf Sediments in Eastern Hainan Island since Middle Holocene

doi: 10.3799/dqkx.2015.134

1.
School of Geosciences, China University of Petroleum, Qingdao 266580, China
2.
Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
3.
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
4.
School of Resources and Geoscience, China University of Mining and Technology, Xuzhou 221008, China

Received Date: 2015-02-25
Publish Date: 2015-09-15

Abstract

Abstract

The influence of Hainan Island has been ignored in the previous researches of sediment provenance in the continental shelf of the northern South China Sea. Therefore, the sediment provenances on the basis of lithology, grain-size, AMS¹⁴C dating, clay mineral analysis that were carried out for Core X2 located in the continental shelf of the Hainan Island in the South China Sea are discussed in the paper. The results show that Core X2 is separated into two stages, namely the upper one and the lower one. The lower one(Ⅰ, 240-120 cm) is mainly composed of clay silt while the upper one (Ⅱ, 120-0 cm) consists mainly of silty sand. Clay minerals in Core X2 mainly consist of illite and kaolinite, with associated chlorite and smectite. The comparison of clay mineral assemblages between sediments at Core X2 and other potential provenances indicates that predominant illite and chlorite may have been originated from Taiwan and the Pearl River, whereas kaolinite may has been provided mainly by Hainan Island and the Pearl River; smectite was derived mainly from Leiqiong area. It shows that materials on Hainan Island have certain influence on the continental shelf in the northern South China Sea. The coarsening of the sediment and the higher content of the kaolinite mean that Hainan Island provides more materials than other provenances in stage Ⅰ, which may have been resulted from climatic variation and enhancement from human activities since 4 ka.
- South China Sea,
- continental shelf,
- grain size,
- clay mineral,
- provenance,
- sediment

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References(54)

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Clay Mineral Characteristics and Provenance of Continental Shelf Sediments in Eastern Hainan Island since Middle Holocene

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