Liang-biao, H. Geochemical study of the core S01 in the South China Sea., Chin. J. Ocean. Limnol. 13, 183–190 (1995). https://doi.org/10.1007/BF02846825
DOI:
Liang-biao, H. Geochemical study of the core S01 in the South China Sea., Chin. J. Ocean. Limnol. 13, 183–190 (1995). https://doi.org/10.1007/BF02846825DOI:
Geochemical study of the core S01 in the South China Sea
摘要
Abstract
Si
Ti
Al
Fe
Mn
Ca
Mg
K
Na
P and Sr
Ba
Rb
Ga
V
Zr
Cr
Ni
Co
Cu
Zn
Pb
Nb
Y
Th
La in the core S01 were analyzed and the pattems of their enrichment are discussed. Enrichment of Na
Fe
Mn
Ba
Cu elements in the core indicates volcanic material are an important source of the sediments in the area. The enrichment frequently varying with the deposition process shows bottom volcanism is frequent in the area and that the studied area is a margin basin with distinct oceanic characteristics. The abnormal enrichment of Mn at the layers (0–15 cm and 665–670 cm) of the core could be closely related to and so
indicate
the wide deposition hiatus that have occurred in the West Pacific Ocean and adjacent margin seas since Late Pleistocene.
关键词
Keywords
references
He Liangbiao, 1992. Clay minerals in the cores from the South China Sea.J. Ocean Univ. Qingdao 22(3): 73–81. (in Chinese with English abstract)
He Liangbiao, 1994. Abnormal enrichment of Mn in the cores from the marginal seas of the Pacific Ocean.Chinese Science Bulletin 39(22): 2110 (in Chinese)
Li Wenqin, Cong Youzi, 1989. The calcareous nannofossils zonation and paleomagnetic dating of cores KS01, KS02 from the centre of the South China Sea.J. Oceanogr. Huanghai & Bohai Seas 7(3): 40–43. (in Chinese with English abstract)
Zhang Fuyuan, 1993. The relation between Ba/Cu ratio in the surface sediments and spreading of the sea floor in the South China Sea.Acta Oceanologica Sinica 15(5): 98–103. (in Chinese)
Zhao Yiyang, Qin Zhaoyang, Li Fengye et al., 1988. A study on element-stratigraphy of Okinawa Trough.Chin. J. Oceanol. Limnol. 6(2): 145–156.
Zhao Yiyang, Yan Mingcai, 1993. The abundances of elements in the sediments from the Chinese shallow seas.Science in China (series B)23(10): 1084–1090. (in Chinese)
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Related Author
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Related Institution
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