| 中国多金属结核开辟区沉积物地球化学特征 |
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| 引用本文： | 倪建宇,周怀阳,潘建明,赵宏樵,扈传昱,王方国.中国多金属结核开辟区沉积物地球化学特征[J].海洋学报,2001,23(6):94-100. |
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| 作者姓名： | 倪建宇 周怀阳 潘建明 赵宏樵 扈传昱 王方国 |
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| 作者单位： | 1.国家海洋局第二海洋研究所, 浙江, 杭州, 310012;国家海洋局第二海洋研究所, 浙江, 杭州, 310012 |
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| 基金项目： | 国家重点基础研究专项经费资助项目(G2000078500);大洋矿产资源勘探开发专项基金资助项目(DY95-06-03). |
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| 摘 要： | 对中国多金属结核开辟区沉积物的详细研究表明,研究区内沉积物处于氧化至弱氧化环境,两种色调的沉积物在粒度分布特征以及化学组成上都存在着显著的差异,它们是不同沉积环境的反应.不同色调之间的界面为一沉积间断面.沉积物中的铁和锰具有不同的来源,铁可能以岩源碎屑为主,而锰则更可能是自生成因.钙和镁以生物成因为主.
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| 关 键 词： | 沉积物组成 多金属结核 赤道太平洋 |
| 文章编号： | 0253-4193(2001)06-0094-07 |
| 收稿时间： | 2000/10/20 0:00:00 |
| 修稿时间： | 2000/12/20 0:00:00 |
Geochemical characteristics of sediments from the China Pioneer Area equatorial northeast Pacific Ocean |
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| NI Jian-yu,ZHOU Huai-yang,PAN Jian-ming,ZHAO Hong-qiao,HU Chuan-yu and WANG Fang-guo.Geochemical characteristics of sediments from the China Pioneer Area equatorial northeast Pacific Ocean[J].Acta Oceanologica Sinica (in Chinese),2001,23(6):94-100. |
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| Authors: | NI Jian-yu ZHOU Huai-yang PAN Jian-ming ZHAO Hong-qiao HU Chuan-yu and WANG Fang-guo |
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| Institution: | 1.Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;Key Laboratory of Submarine Geosciences of State Oceanic Administration, Hangzhou 310012, China2.Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China |
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| Abstract: | In the China Pioneer Area, located in the western part of the area between the Clarion and Clipperton Fraction Zones, the topmost sediment column can be divided into two layers based on distinctive color and bioturbation properties: an upper pale brown layer (Unit A) and a lower dark brown layer (Unit B). Chemical properties in Unit A and Unit B are clearly different across the color boundary, which can be interpreted to be a hiatus. This results in an overall difference in sediment properties between Unit A and Unit B, that is, older Unit B sediment is higher in P 2O 5, MnO 2, CaO and Na 2O contents. Based on the correlation analysis, Mn and Fe in sediments have different genesis. The manganese mainly is authigenes, but Fe is from rock weathering. Therefore, the chemical differences in sediments are the results of sedimentation setting differences. |
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| Keywords: | sediment component multimetallic nodules equatorial Pacific Ocean |
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