海洋铁锰结壳中碲的富集过程研究进展  

Progress on tellurium enrichment in the ocean ferromanganese crusts

作　　者：孙阳 崔迎春 马立杰[2] 方习生 张浩 陈绍聪 宗师 王伟轩 王庆超 SUN Yang;CUI Yingchun;MA Lijie;FANG Xisheng;ZHANG Hao;CHEN Shaocong;ZONG Shi;WANG Weixuan;WANG Qingchao(Key Laboratory of Polar Science,Ministry of Natural Resources,Polar Research Institute of China,Shanghai 201209,China;Key Laboratory of Marine Geology and Environment,Chinese Academy of Science,Institute of Oceanology of Chinese Academy of Science,Shandong Qingdao 266071,China;Lab of Marine Geology and Geophysics,First Institute of Oceanography,Shandong Qingdao 266061,China)

机构地区：[1]中国极地研究中心,自然资源部极地科学重点实验室,上海201209 [2]中国科学院海洋研究所中国科学院海洋地质与环境重点实验室,山东青岛266071 [3]自然资源部第一海洋研究所海洋地质与地球物理研究室,山东青岛266061

出　　处：《中国地质调查》2023年第4期65-71,共7页Geological Survey of China

基　　金：国家自然科学基金“西太平洋海山铁锰结壳发育程度相关的海底图谱(编号:42276080)”“富钴结壳生长界面对其成矿过程的制约(编号:40706029)”“西太平洋俯冲带水的赋存、迁移以及与岩石圈相互作用机理研究(编号:91958216)”以及“基于航空地球物理探测的东南极Lambert裂谷——Amery冰架地区冰下环境与地质结构研究(编号:41876227)”项目联合资助。

摘　　要：碲(Te)元素在工业生产中被广泛应用,但在地壳中含量极低,在海洋铁锰结壳中高度富集。评述了海洋铁锰结壳中Te富集过程的相关研究,结果表明:Te在全球海洋中的分布存在空间差异,其中印度洋东经90°海岭铁锰结壳中的Te含量表现出由南向北逐渐升高的特征;铁锰结壳中更古老壳层的Te含量更高,结壳中Te的物质通量会随壳层生长速率的变化而改变;Te以多种形式赋存在铁锰结壳中,且来源具有多源性,主要通过物理过程和化学过程进入结壳。研究有助于促进分散元素海底成矿理论的发展。The element tellurium is widely used in industrial production,but it is depleted in the earth's crust and riched in oceanic ferromanganese crusts.The authors in this paper reviewed the study about the enrichment process of tellurium in ferromanganese crusts,and it is found that the tellurium content in ferromanganese crusts in various regions is different.For example the tellurium in the E 90° ridge region in Indian Ocean with the increasing trends from north to south.Temporally,the content of tellurium in the old crust is higher,and the tellurium flux would vary with the growh ratios of crusts.The Tellurium element occurs as multi-mineral phases and has multi-sources in ferromanganese crusts,which is controlled by the oceanic physical and chemical process.This research would be beneficial to the development of mineralization theory of dispersed elements.

关 键 词：铁锰结壳 Te元素 赋存状态 物质来源 富集机制 

分 类 号：P744.3[天文地球—海洋科学]