The preliminary research on element distribution for micro-structure in seamount Co-rich crust using SR-XRMP

WANG Xiaohong1; 2 ZHAN Xiuchun1 HUANG Yuying3 HE Wei3 LIU Shuqin4 FAN Xingtao1 TANG Lijun1 WANG Yimin1 1

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The preliminary research on element distribution for micro-structure in seamount Co-rich crust using SR-XRMP

更新时间：2021-03-12

- The preliminary research on element distribution for micro-structure in seamount Co-rich crust using SR-XRMP
- NUCLEAR TECHNIQUES Issue 11, (2005)
- 作者机构：
  
  1. 国家地质实验测试中心
  2. 中国地质科学院
  3. 中国科学院高能物理研究所
  4. 矿产资源研究所
  5. 中国地质科学院北京100037北京大学环境学院北京,100871
  6. ,北京,100049
- 作者简介：
- 基金信息：
  
  “大洋”协会国际海底区域研究开发“十五”专项基金(DY105-01-04-05);国土资源部百名优秀青年科技人才计划北京正负电子对撞机国家实验室重点课题资金共同资助
- DOI：
  CLC： P736.4
- Published：01 November 2005
- 稿件说明：
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[1]王晓红,詹秀春,黄宇营,何伟,刘淑琴,樊兴涛,唐力军,王毅民.SR-XRMP研究海山富钴结壳微构造的元素分布特征[J].核技术,2005(11):4-9.

WANG Xiaohong1, 2 ZHAN Xiuchun1 HUANG Yuying3 HE Wei3 LIU Shuqin4 FAN Xingtao1 TANG Lijun1 WANG Yimin1 1. The preliminary research on element distribution for micro-structure in seamount Co-rich crust using SR-XRMP[J]. Nuclear techniques, 2005, (11).
[1]王晓红,詹秀春,黄宇营,何伟,刘淑琴,樊兴涛,唐力军,王毅民.SR-XRMP研究海山富钴结壳微构造的元素分布特征[J].核技术,2005(11):4-9. DOI：

WANG Xiaohong1, 2 ZHAN Xiuchun1 HUANG Yuying3 HE Wei3 LIU Shuqin4 FAN Xingtao1 TANG Lijun1 WANG Yimin1 1. The preliminary research on element distribution for micro-structure in seamount Co-rich crust using SR-XRMP[J]. Nuclear techniques, 2005, (11). DOI：

摘要

海山富钴结壳具有与大洋锰结核相似的叠层石微构造

蕴含着与古海洋环境相关的丰富信息。本文用同步辐射X射线微探针研究了采自西太平洋海山区两个富钴结壳样品剖面的多种微结构及其主要成矿元素的微区分布特征

揭示了结壳在漫长的生长过程中Mn、Fe、Co、Ni、Cu、P和Ca的相关关系的变化及古海洋学意义

这些变化特征可作为重要古海洋事件——磷酸盐化的判别依据。

Abstract

Seamount Co-rich crust has the same stromatolithic structure with marine manganese nodule. It contains rich information of paleoceanic environment recorded during its growth period. In this paper

the distribution features of the main mineral-forming elements Mn

P and Ca in two seamount Co-rich crusts

collected from the west Pacific

have been studied using SR-XRMP. These distribution features of main mineral-forming elements can be used as the tracer for phosphatization ( an important paleoceanic event ) .

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