中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The Genesis and Geological Implications for Oceanic Redbeds of the South China Sea in U1434 of IODP Expedition 349-the Constraint from Diffuse Reflectance and X-Ray Fluorescence Spectroscopy

文献类型:期刊论文

作者Li Jian5; Tang Qin-gin; Zhan Wen-huan; Hu Li-tian; Sun Jie; Jiang Lian-ting
刊名SPECTROSCOPY AND SPECTRAL ANALYSIS
出版日期2019
卷号39期号:4页码:1294
关键词Oceanic redbeds Theraml origin Oxygen fugacity South China Sea
ISSN号1000-0593
DOI10.3964/j.issn.1000-0593(2019)04-1294-07
英文摘要We presented a new finding that the occurrences of oceanic redbeds in the South China Sea (SCS) first discovered from Expedition 349 are similar to those in Sulu Sea and Celebes Sea from Expedition 124, as well as to the continental redbeds in Sanshui Basin of China, all directly covering massive magmatic rocks with significance for revealing the connections between oceanic redbeds and magma thermal events. We measured the samples collectted from marine sedimentary with colors ranging from celadon to rufous in U1434 of IODP Expedition 349, and analyzed the influence of oxygen fugacity and geothermal temperature on the formation of pigment in redbeds. By comparing red-nonred sediments and experimental samples, we discussed the redbed genesis and its geological implications. We obtained the red values, the content of goethite, hematite and quantivalent Fe in marine sediments and experiment samples through the analysis of diffuse reflectance and fluorescent spectroscopy and Fe2+ in titration test. The results showed that, (1) Red and non-red marine sediments are formed at high oxygen fugacity environment in U1434 of IODP Expedition 349, and difference in oxidation-deoxidation environment was not the controlling factor on red and non-red sediments; (2) The oceanic redbeds directly covering basalts in U1434 of IODP Expedition 349 originated from high geothermal temperature during sedimentary-diagenesis process; (3) And we found that continental redbeds and Cretaceous oceanic redbeds formed in different geological periods are closely associated with tectonic-magmatic active belts, showing that redbeds have significance in indicating geological thermal events.
源URL[http://ir.scsio.ac.cn/handle/344004/17968]  
专题南海海洋研究所_中科院边缘海地质重点实验室
作者单位1.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangzhou 510275, Guangdong, Peoples R China
2.[Jiang Lian-ting
3.Sun Jie
4.Zhan Wen-huan
5.Tang Qin-gin
6.Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China
7.Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangdong Prov Key Lab Geodynam & Geohazards, Guangzhou 510275, Guangdong, Peoples R China
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GB/T 7714
Li Jian,Tang Qin-gin,Zhan Wen-huan,et al. The Genesis and Geological Implications for Oceanic Redbeds of the South China Sea in U1434 of IODP Expedition 349-the Constraint from Diffuse Reflectance and X-Ray Fluorescence Spectroscopy[J]. SPECTROSCOPY AND SPECTRAL ANALYSIS,2019,39(4):1294, 1300.
APA Li Jian,Tang Qin-gin,Zhan Wen-huan,Hu Li-tian,Sun Jie,&Jiang Lian-ting.(2019).The Genesis and Geological Implications for Oceanic Redbeds of the South China Sea in U1434 of IODP Expedition 349-the Constraint from Diffuse Reflectance and X-Ray Fluorescence Spectroscopy.SPECTROSCOPY AND SPECTRAL ANALYSIS,39(4),1294.
MLA Li Jian,et al."The Genesis and Geological Implications for Oceanic Redbeds of the South China Sea in U1434 of IODP Expedition 349-the Constraint from Diffuse Reflectance and X-Ray Fluorescence Spectroscopy".SPECTROSCOPY AND SPECTRAL ANALYSIS 39.4(2019):1294.

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来源:南海海洋研究所

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