铁陨石

青岛铁陨石是在2004年5月发现于青岛市城阳区惜福镇，重约30t。

The Qingdao iron meteorite was found in May , 2004.Its weight is about 3 ton .

指出南丹铁陨石似分为IAB群较合理，它可能是由具有球粒陨石组成的母源物质受冲击、经局部熔融而形成。

It seems reasonable that the Nandan iron meteorite should be classified to the group IAB . Further , it might be formed from the source matter with the chondritic composition , which experienced the impact and partial melting .

地球的初始物质为分异的铁陨石及H群球粒陨石。

The primitive material of the Earth were the differentiated iron meteorites and H chondrites .

南丹铁陨石冲击绝热线和状态方程的研究

Studies on the shock adiabatics and equation-of-state of Nandan iron meteorite

未分群铁陨石及其硅酸盐包体的研究

A Study of the Ungrouped Iron Meteorite and Its Silicate Inclusion

35个铁陨石化学组成研究及其在分类学中的应用

Chemical compositional study of 35 iron meteorites and its application in taxonomy

铁陨石及中铁陨石的稀有气体同位素丰度和放射性核素活度

Noble gas isotopic abundances and radionuclide activities of iron meteorites and mesosiderites

新疆铁陨石的矿物学特征及其母体形成条件

Mineralogical features of Xinjiang iron meteorite and forming conditions of its parent body

中国某些铁陨石的化学分类

The compositional classification of some Chinese iron meteorites

我的意思是，找铁陨石更简单。

I mean , it 's easier to find an iron meteorite or stony iron .

我国铁陨石研究

Studies of iron meteorites in China

南极GRV98003和其它3个铁陨石的化学组成及分类

Chemical compositions and classification of Grove Mountains ( grv ) 98003 and other three iron meteorites

宁波铁陨石宇宙成因核的测定

γ - ray spectrometric measurements on the Ningbo iron meteorite for its radioactive species produced by cosmic ray

测试发现这些珠宝包含非地球矿石的踪迹，这些矿石只在富铁陨石中发现过。

The tests revealed that the jewelry contained trace elements not present in Earthly ores - but that are found in iron-rich meteorites .

作者详细观测研究了新疆铁陨石24块不同取样点样品的矿物组成、化学成分和结构构造特征。

The mineral composition , chemical composition and textural features of 24 surface samples of the Xinjiang iron meteorite taken at different positions have been investigated in detail .

近40年来陨石分类学经历了3个发展阶段：60～70年代，由根据陨石的矿物结构的分类方法发展为球粒陨石的化学&岩石学分类法和铁陨石的化学群分类法；

In recent 40 years , meteorite taxology has undergone three development stages . In the 1960-1970s , chemical petrologic classification of chondrites and chemical classification of iron meteorite were established .