铁族元素

研究还发现重矿物、碳酸盐、某些微量元素以及过渡金属元素，如铁族元素Fe、Mn、V、Cr、Ni和亲铜元素Cu、Zn等在判别沉积物长江、黄河源属性方面比较有效；

We also find that heavy minerals , carbonate , some trace elements and transitive metals , such as Fe , Mn , V , Cr , Ni , Cu , Zn are effective in discriminating the origin of the sediment , from Yangtze River or Yellow River ?

在元素地球化学分类中，钛属铁族元素，在内生作用过程中；

Titanium belongs to Ferrum earth family in geochemical element classification .

本文对取自西菲律宾海区的三个柱状沉积物岩芯的铁族元素地球化学行为进行了系统的研究。

The geochemistry of iron group elements sampled from three cores in the West Philippine Sea is studied systematically and comprehensively .

钨钼族元素的低背景与铁族元素、亲铜元素的低背景之间的过渡带为铀矿床的有利富集地带；

The transitional zones between low backgrounds of W Mo group elements and iron group and chalcophile elements are the favorable enriched zones of uranium deposits .

铁族元素是元素周期表中非常重要的一族元素，纳米尺度的铁族元素的研究更是材料研究领域的热点之一。

Iron group elements are very important in the periodic table , and the related research on nanometer scale is the hotspot in the fields of materials science .

锰是地壳中最主要的20种元素之一，与其它同属铁族元素相比，锰在矿物学、地球化学、矿床学等特征上要复杂得多，其地球化学行为也复杂得多。

The manganese is one of the major element in the earth , comparison with other Fe-group element , it has more complicated characteristic in mineralogy , geochemistry and ore deposit .

从元素的含量及剖面变化、元素的相关性及组合特征，铁族元素与主元素的关系以及元素的赋存状态等方面探讨了物质来源、沉积作用和古气候，并据此进行了地层划分。

The origin of sediments , sedimentation process and paleoclimate are discussed , and the stratigraphy is classified , based on the concentrations of elements , their variations in profiles , the relationship of iron group elements with the main elements , and the storage status .

富Co铁锰结壳铂族元素与铼-锇同位素组成及其意义

PGE and Re-Os isotope compositions and their significances of Co-rich ferromanganese crusts

根据该反应机理，这种微波辅助多元醇溶剂法有可能扩展应用于铁的其它硫族元素化合物例如FeS、FeTe、（FeSSe）、Fe（SeTe）等的合成中。

This microwave-assisted polyol approach can be potentially extended to synthesis of other iron chalcogenides , such as FeS , FeTe , ( FeSSe ) and Fe ( SeTe ) .