Combination Distribution Characteristics and Corresponding Material Sources of Surface Clay Minerals in Beibu Gulf, China

Na Zhang; Yu Tong Yan; Sheng Rong Li; Xiu Yun Tong; Li Na Yan

doi:10.4028/www.scientific.net/AMR.616-618.158

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 616-618Combination Distribution Characteristics and...

Combination Distribution Characteristics and Corresponding Material Sources of Surface Clay Minerals in Beibu Gulf, China

Abstract:

Clay minerals are the main ingredients of the ocean floor sediments, which completely record a lot of geological information and have important meanings in the studies of source material, sedimentary environment, global climate change, sea-level fluctuation and ocean currents evolution. This paper studies composition and combination distribution characteristics of 312 surface clay mineral samples and makes the mineral mapping in Beibu gulf. The results show that the components of clay minerals in Beibu gulf are mainly mixed layer of illite and montmorillonite, kaolinite, chlorite and illite and each average content are 49.95%, 24.69%, 14.07% and 11.28%, respectively. According to combination and content of the clay minerals, the distribution areas of clay minerals in Beibu gulf can be divided into four divisions of 1, 2, 3 and 4 divisions. The differences of 4 divisions are closely related with the source area parent rocks and circulation.

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Periodical:

Advanced Materials Research (Volumes 616-618)

Pages:

158-161

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.616-618.158

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Online since:

December 2012

Authors:

Na Zhang, Yu Tong Yan, Sheng Rong Li, Xiu Yun Tong, Li Na Yan

Keywords:

Beibu Gulf, Clay Mineral, Distribution Characteristics, Mineral Combination

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References

[1] Rowan ,K. S. . Photosynthetic Pigments of Algea. New York : Cambridge University Press , 1989. 166-189

Google Scholar

[2] Glazer ,A. N. . Photosynthetic Accessory Proteins with Bilin Prosthetic Groups.In : Hatch ,M. D. and Boardman ,N. K. eds. The Biochemistry of Plants.New York :Academic Press. 1981. 8 :51-96

DOI: 10.1016/b978-0-12-675408-7.50008-2

Google Scholar

[3] Rowan ,K. S. . Photosynthetic Pigments of Algea. New York : Cambridge University Press , 1989. 166～189

Google Scholar

[4] Glazer ,A. N. . Photosynthetic Accessory Proteins with Bilin Prosthetic Groups.In : Hatch ,M. D. and Boardman ,N. K. eds. The Biochemistry of Plants.New York :Academic Press. 1981. 8 :51-96

DOI: 10.1016/b978-0-12-675408-7.50008-2

Google Scholar

[5] Revelle, R., Marine bottom samples collected in the Pacific Ocean by the CARNEGIE on its seventh cruise, Carnegie Inst., Washington Publication.

DOI: 10.1086/394997

Google Scholar

[6] Wu WZ, Zhu YZ. Clay minerals in South sea [J]. Tropical ocean,1983, 2(1):20-27.(In Chinese with English abstract).

Google Scholar

[7] Li GG. Composition, distribution and geological significance of offshore surface sediments [J]. Marine Journal, 1990, 12(4):470-479. (In Chinese with English abstract).

Google Scholar

[8] Chen LR, Zhang XR. Composition and distribution in Beibu gulf [J]. Marine Journal, 1986， 8(3):340-346. (In Chinese with English abstract).

Google Scholar

[9] Xu DY, Liu XQ, Zhang XH, et al. Offshore geology in China. Geology Press. 1997.

Google Scholar

[10] Li M J, Wang T G, Liu J, et al. Occurrence and origin of carbon dioxide in the Fushan Depression, Beibuwan Basin, South China Sea. Marine and Petroleum Geology, 2008,25:500-513. [1] Boyle R. (1979). The geochemistry of gold and its deposits[M]. Canada: Canada Geological Survey Bulletin.

DOI: 10.1016/j.marpetgeo.2007.07.007

Google Scholar