青岛铁陨石的发现及其化学成分和矿物学分析

尹延鸿; 孙嘉诗; 刘昌岭; 刘新波; 马新国

青岛铁陨石的发现及其化学成分和矿物学分析

1 青岛海洋地质研究所, 青岛 266071;
2 青岛琴岗监理公司, 青岛 266071

基金项目:

国家自然科学基金项目(40272078)

详细信息

作者简介:
尹延鸿(1954-),男,研究员,从事海洋地质、构造地质和环境地质研究

中图分类号: P68
计量
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出版历程
- 收稿日期: 2005-10-12
- 修回日期: 2006-02-27

THE DISCOVERY OF QINGDAO IRON METEORITE AND ITS CHEMIEAL COMPOSITION AND MINERALOGY

1 Qingdao Institute of Marine Geology, Qingdao 266071, China;
2 Qingdao Qingang Supervise Company, Qingdao 266071, China

摘要

摘要: 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30 t。通过初步的化学分析和矿物学分析,发现其铁含量为94.02%,镍含量为5.29%,钴含量为0.45%,主要矿物为铁纹石,局部含有陨磷铁镍石的晶体或集合体,表明它是一块典型的铁陨石。该区历史上没有陨石降落的记载,根据该铁陨石产出在第四系的全新世冲-洪积层中离地表3~4 m的深度处,推断它的降落年代应是全新世。
- 铁陨石 /
- 化学成分 /
- 矿物学特征 /
- 铁纹石 /
- 青岛
Abstract: The Qingdao iron meteorite was found in May,2004.Its weight is about 3 ton.It may be the third largest iron meteorite in China.Fe content is 94.02%,Ni content 5.29%,and Co 0.45% in the iron meteorite.The main mineral is kamacite,and crystal and aggregate of schreibersite were also found in the iron meteorite.These minerals are typical of iron meteorite.The iron meteorite occurred in Holocene sediments,so it landed in Holocene.
- meteorite /
- chemical composition /
- mineralogy /
- Qingdao

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参考文献(9)

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