东菲律宾海深水区新型铁锰结壳的特征和成因
对取自东菲律宾海深水区致密-半固结沉积物表层的新型铁锰结壳典型样品进行了X射线衍射、X射线荧光、电感耦合等离子体原子发射光谱及加速器质谱研究。结壳的组成矿物主要有δMnO2、铁的氧化物/氢氧化物、石英、长石和黏土矿物等。与海山结壳相比,其Mn、Co、Ni、Zn、Pb含量均较低,而Fe、Cu、Al含量则相对较高。Mn/Fe值平均仅为0.24,也低于海山结壳Mn/Fe的平均值。相关性分析、元素分配系数分析及稀土元素北美页岩标准化配分模式等结果均表明,研究区结壳为一新型边缘海深水水成结壳,与海山水成结壳间存在一定差异。结壳的物质组分主要来自于同期海水,同时碎屑物质对其形成也有一定贡献;并且它们自形成...
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| Published in | Hăiyang dĭzhĭ yu dĭsĭjĭ dĭzhĭ Vol. 26; no. 4; pp. 91 - 98 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | Chinese |
| Published |
Beijing
Marine Geology and Quaternary Geology
01.01.2006
中国科学院,海洋地质与环境重点实验室,中国科学院海洋研究所,青岛,266071 中国科学院,研究生院,北京,100039%中国科学院,海洋地质与环境重点实验室,中国科学院海洋研究所,青岛,266071 |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0256-1492 |
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| Abstract | 对取自东菲律宾海深水区致密-半固结沉积物表层的新型铁锰结壳典型样品进行了X射线衍射、X射线荧光、电感耦合等离子体原子发射光谱及加速器质谱研究。结壳的组成矿物主要有δMnO2、铁的氧化物/氢氧化物、石英、长石和黏土矿物等。与海山结壳相比,其Mn、Co、Ni、Zn、Pb含量均较低,而Fe、Cu、Al含量则相对较高。Mn/Fe值平均仅为0.24,也低于海山结壳Mn/Fe的平均值。相关性分析、元素分配系数分析及稀土元素北美页岩标准化配分模式等结果均表明,研究区结壳为一新型边缘海深水水成结壳,与海山水成结壳间存在一定差异。结壳的物质组分主要来自于同期海水,同时碎屑物质对其形成也有一定贡献;并且它们自形成以来没有遭受明显的成岩后期改造和元素再迁移,具有较高的古海洋学应用价值。 |
|---|---|
| AbstractList | 对取自东菲律宾海深水区致密-半固结沉积物表层的新型铁锰结壳典型样品进行了X射线衍射、X射线荧光、电感耦合等离子体原子发射光谱及加速器质谱研究。结壳的组成矿物主要有δMnO2、铁的氧化物/氢氧化物、石英、长石和黏土矿物等。与海山结壳相比,其Mn、Co、Ni、Zn、Pb含量均较低,而Fe、Cu、Al含量则相对较高。Mn/Fe值平均仅为0.24,也低于海山结壳Mn/Fe的平均值。相关性分析、元素分配系数分析及稀土元素北美页岩标准化配分模式等结果均表明,研究区结壳为一新型边缘海深水水成结壳,与海山水成结壳间存在一定差异。结壳的物质组分主要来自于同期海水,同时碎屑物质对其形成也有一定贡献;并且它们自形成以来没有遭受明显的成岩后期改造和元素再迁移,具有较高的古海洋学应用价值。 P744.3; 对取自东菲律宾海深水区致密-半固结沉积物表层的新型铁锰结壳典型样品进行了X射线衍射、X射线荧光、电感耦合等离子体原子发射光谱及加速器质谱研究.结壳的组成矿物主要有δMnO2、铁的氧化物/氢氧化物、石英、长石和黏土矿物等.与海山结壳相比,其Mn、Co、Ni、Zn、Pb含量均较低,而Fe、Cu、Al含量则相对较高.Mn/Fe值平均仅为0.24,也低于海山结壳Mn/Fe的平均值.相关性分析、元素分配系数分析及稀土元素北美页岩标准化配分模式等结果均表明,研究区结壳为一新型边缘海深水水成结壳,与海山水成结壳间存在一定差异.结壳的物质组分主要来自于同期海水,同时碎屑物质对其形成也有一定贡献;并且它们自形成以来没有遭受明显的成岩后期改造和元素再迁移,具有较高的古海洋学应用价值. |
| Author | Qing-yong, MENG An-chun, LI Zhao-kai, XU Jian-guo, LIU Fu-qing, JIANG |
| AuthorAffiliation | 中国科学院,海洋地质与环境重点实验室,中国科学院海洋研究所,青岛,266071;中国科学院,研究生院,北京,100039%中国科学院,海洋地质与环境重点实验室,中国科学院海洋研究所,青岛,266071 |
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| Title | 东菲律宾海深水区新型铁锰结壳的特征和成因 |
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