Skip to main content

Iron meteorites

  • Reference work entry
Encyclopedia of Planetary Science

Part of the book series: Encyclopedia of Earth Science ((EESS))

  • 43 Accesses

Iron meteorites are perhaps the most spectacular samples of extraterrestrial materials, and may be the ones known to humanity for the longest time. Prehistoric humans used meteoritic iron as raw material for tools and artefacts. Some iron meteorites may have been venerated as sacred objects.

The abundance of iron meteorites in museum collections is not due to a high incidence of iron meteorite falls. Among the roughly 900 observed meteorite falls there are less than 50 irons. Most of the over 700 known iron meteorites owe their preservation to the fact that they weather more slowly and are more conspicuous to human collectors than other types of extraterrestrial rocks. A comprehensive overview of known iron meteorite samples has been given by Buchwald (1975).

Metallography and mineralogy

The major component of iron meteorites is nickel—iron (Fe, Ni), although practically all of them also contain various minor phases. The metal usually contains 5–15% Ni by weight, but samples with up to...

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Institutional subscriptions

Bibliography

  • Buchwald, V. F. (1975) Handbook of Iron Meteorites, 3 vols. Berkeley: University of California Press.

    Google Scholar 

  • Chen, J. H. and Wasserburg, G. J. (1990) The isotopic composition of Ag in meteorites and the presence of 107Pd in protoplanets. Geochim. Cosmochim. Acta, 54, 1729–43.

    Google Scholar 

  • Saikumar, V. and Goldstein, J. I. (1988) An evaluation of the methods to determine the cooling rates of iron meteorites. Geochim. Cosmochim. Acta, 52, 715–26.

    Google Scholar 

  • Scott, E. R.D. (1972) Chemical fractionation in iron meteorites and its interpretation. Geochimica Cosmochim. Acta, 36, 1205–36.

    Google Scholar 

  • Swartzendruber, L. J., Itkin, V. P. and Alcock, C. B. (1991) Fe—Ni (iron—nickel), in Phase Diagrams of Binary Nickel Alloys (ed. P. Nash). Material Park, OH: ASM International, pp. 110–132.

    Google Scholar 

  • Voshage, H. (1967) Bestrahlungsalter und Herkunft der Eisenmeteorite. Z. Naturforsch, 22a, 477–506.

    Google Scholar 

  • Wasson, J. T. (1974) Meteorites: Classification and Properties. Berlin and New York: Springer-Verlag.

    Google Scholar 

  • Wasson, J. T. (1985) Meteorites: Their Record of Early Solar-System History. New York: W.H. Freeman.

    Google Scholar 

  • Wasson, J. T., Ouyang, X., Wang, J. and Jerde, E. (1989) Chemical classification of iron meteorites — XI. Geochim. Cosmochim. Acta, 53, 735–44.

    Google Scholar 

Cross references

Download references

Authors

Rights and permissions

Reprints and permissions

Copyright information

© 1997 Chapman & Hall

About this entry

Cite this entry

Kracher, A. (1997). Iron meteorites . In: Encyclopedia of Planetary Science. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4520-4_197

Download citation

  • DOI: https://doi.org/10.1007/1-4020-4520-4_197

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-412-06951-2

  • Online ISBN: 978-1-4020-4520-2

  • eBook Packages: Springer Book Archive

Publish with us

Policies and ethics