深海沉积物中碲异常的成因
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引用本文:李傲仙,李延河,乐国良.2005.深海沉积物中碲异常的成因[J].地球学报,26(z1):186-189.
DOI:10.3975/cagsb.2005.s1.59
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作者单位E-mail
李傲仙 石油大学北京102249 aoxianli@pepris.com 
李延河 国土资源部同位素地质重点实验室北京100037中国地质科学院矿产资源研究所北京100037  
乐国良 国土资源部同位素地质重点实验室北京100037中国地质科学院矿产资源研究所北京100037  
基金项目:国家自然科学基金项目(编号:4987300和国土资源部科技项目(编号:20010209)联合资助
中文摘要:碲在地球上是一种稀有分散元素,碲在地壳中的丰度很低,仅为1.0ng/g;但碲在富钴结壳、海底多金属结核、党海沉积物和陨石中的丰度异常高。为了查明深海沉积物中碲异常的原因,笔者对比分析了深海沉积物中磁性部分与全岩的碲含量和氦同位素组成。结果显示磁性部分的He含量和3He/4He比值及Te含量较全岩的值明显偏高;3He含量与Te含量同步变化;在3He-Te关系图上,二者具明显的正相关关系。本文首次提出深海沉积物中的碲异常与氦同位素异常一样可能是由宇宙尘注入引起的;海底多金属结核和富钴结壳中的碲异常可能也与宇尘有关。
中文关键词:深海沉积物 碲含量异常 氦同位素 宇宙尘
 
The Cause for Tellurium Enrichment in Deep-Sea Sediments
Abstract:Tellurum is a sort of scattered rare elements in the earth. Its concentration seems very low in the earth's crust,being only 1.0ng/g. However, tellurium contents are extrmely high in Co-rich crusts, marine polymetallic nodules,deep-sea sediments and aerolites. To find out the causes for tellurium enrichments in deep-sea sediments,the authors analyzed and compared tellurium concentrations and helium isotope compositions in the magnetic parts and those in the bulk samples of deep-sea sediments. Helium contents,3He/4He ratios and tellurium concentrations are obviously higher in the magnetic parts than in the bulk samples.3He abundances synchronously vary with tellurium concentrations.3He-Te has distinct positive correlation with each other. This paper puts forward for the first time the opinion that the extreme enrichment of tellurium in deep-sea sediments,like helium isotope anomalies, probably results from the input of inerplanetary dust particles(IDPs).Similarly the extreme enrichments of tellurium in marine polymetallic nodules and Co-rich crusts are possibly related to IDPs.
keywords:deep=sea sediments extreme enrichment of tellurium helium isotope interplanetary dust particles(IDPs)
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