Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-22T15:55:16.899Z Has data issue: false hasContentIssue false
  • English
  • Français

Orientation relationships of carlsbergite in schreibersite and kamacite in the north Chile iron meteorite

Published online by Cambridge University Press:  05 July 2018

G. Nolze ,
G. Wagner ,
R. Saliwan Neumann ,
R. Skála  and
V. Geist
G. Nolze*
Affiliation:
Federal Institute for Materials Research and Testing, Unter den Eichen 87, 12205 Berlin, Germany
G. Wagner
Affiliation:
Institute for Mineralogy, Crystallography and Materials Science, University of Leipzig, Scharnhorststrasse 20, 04275 Leipzig, Germany
R. Saliwan Neumann
Affiliation:
Federal Institute for Materials Research and Testing, Unter den Eichen 87, 12205 Berlin, Germany
R. Skála
Affiliation:
Institute of Geology, Academy of Sciences of the Czech Republic, Rozvojová 135, CZ-16502 Prague, Czech Republic
V. Geist
Affiliation:
Institute for Mineralogy, Crystallography and Materials Science, University of Leipzig, Scharnhorststrasse 20, 04275 Leipzig, Germany
*
*E-mail: [email protected]
Get access Rights & Permissions [Opens in a new window]

Abstract

The crystallographic orientation of carlsbergite (CrN) in the north Chile meteorite (hexahedrite) was investigated using electron backscatter diffraction and transmission electron microscopy. These studies examined the CrN crystals in the rhabdites (idiomorphic schreibersite) and in kamacite. It was found that the CrN crystals embedded in rhabdite show a number of different orientation relationships with the host crystals. These orientations can be explained based on the lattice dimensions of both coexisting crystalline materials. It was also found that both carlsbergite and kamacite are characterized by a high dislocation density (≥ l09 cm-2) while rhabdite is free of dislocations. It is supposed that in spite of the deformed metallic matrix, a general connection between the orientation relation of all the phases involved exists.

Keywords

EBSDphosphidescarlsbergiteorientation relationshipiron meteorites
Type
Editorial
Information
Mineralogical Magazine , Volume 70 , Issue 4 , August 2006 , pp. 373 - 382
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2006

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Axon, H. J., Kinder, J., Haworth, C. W. and Horsfield, J. W. (1981) Carlsbergite, CrN, in troilite, FeS, of the Sikhote Alin meteoritic iron. Mineralogical Magazine, 44, 107–109.CrossRefGoogle Scholar
Bøggild, O. B. (1927) The meteoritic iron from Savik near Cape York. Meddelelser om Gronland, 74, 11–30.Google Scholar
Buchwald, V. F. (1975) Handbook of Iron Meteorites. University of California Press, USA, 1375 pp.Google Scholar
Buchwald, V. F. and Scott, E. R. D. (1971) First nitride (CrN) in iron meteorites. Nature Physical Science, 233, 113–114.CrossRefGoogle Scholar
Clarke, R. S. and Goldstein, J. I. (1978) Schreibersite growth and its influence on the metallography of coarse-structured iron meteorites. Smithsonian Contribution to Earth Science,. Report no 21, Smithsonian Institution.CrossRefGoogle Scholar
Doenitz, F. D. (1970) Die Kristallstruktur des meteor- itischen Rhabdites (Fe,Ni)3P. Zeitschrift fürr Kristallographie, 131, 222–236.CrossRefGoogle Scholar
Fultz, B. and Howe, J. M. (2005) Transmission Electron Microscopy and Diffractometry of Materials. Springer Berlin, 748 pp.Google Scholar
Geist, V., Wagner, G., Nolze, G. and Moretzki, O. (2005) Investigation of the meteoritic mineral (Fe,Ni)3P. Crystal Research and Technology, 40, 52–64.CrossRefGoogle Scholar
Grady, M. M., editor (2000) Catalogue of Meteorites. Cambridge University Press, Cambridge, UK, 689 pp.Google Scholar
He, Y., Godet St., P.JJ and Jonas, J. J. (2006) Crystallographic relations between face-and body-centred cubic crystals formed under near-equilibrium conditions: Observations from the Gibeon meteorite. Ada Materialia, 54, 1323–1334.Google Scholar
Headley, T. J. and Brooks, J. A. (2002) A new bcc-fcc orientation relationship observed between ferrite and austenite in solidification structures of steels. Metallurgical and Materials Transactions, A33, 5–15.CrossRefGoogle Scholar
Hennig, C., Geist, V. and Heide, G. (1999) Investigation of the rhabdite/kamacite law of intergrowth in iron meteorites with the aid of the Kossel effect. Meteoritics and Planetary Science, 34, 61–66.CrossRefGoogle Scholar
Hölzel, A. R. (1989) Systematics of Minerals. Published by the author, Mainz, Germany, 584 pp.Google Scholar
Leroux, H. (2001) Micro structural shock signatures of major minerals in meteorites. European Journal of Mineralogy, 13, 253–272.CrossRefGoogle Scholar
Moretzki, O., Morgenroth, W., Skála, R., Szymanski, A., Wendschuh, M. and Geist, V. (2005) Determination of the metal ordering in meteoritic (Fe,Ni)3 P crystals. Journal of Synchrotron Radiation, 12, 234–240.CrossRefGoogle Scholar
Nasreddine, M., Bertaut, E. F., Roubin, M. and Paris, J. (1977) Crystallographic study of low-temperature CrxV1-xN. Ada Crystallographica, B33, 3010–3013.Google Scholar
Nolze, G. and Geist, V. (2004) A new method for the investigation of orientation relationships in meteoritic plessite. Crystal Research and Technology, 39, 343–352.CrossRefGoogle Scholar
Nolze, G., Geist, V., Saliwan Neumann, R. and Buchheim, M. (2005) Investigation of orientation relationships by EBSD and EDS on the example of the Watson iron meteorite. Crystal Research and Technology, 40, 791–804.CrossRefGoogle Scholar
Nye, J. F. (2000) Physical Properties of Crystals. Clarendon Press, Oxford, UK, 329 pp.Google Scholar
Randich, E. and Goldstein, J. I. (1978) Cooling rates of seven hexahedrides. Geochimica et Cosmochimica Ada, 42, 221–233.CrossRefGoogle Scholar
Schwartz, A. J., Kumar, M. and Adams, B. L. (2000) Electron Backscatter Diffraction in Material Science. Springer, The Netherlands, 350 pp.CrossRefGoogle Scholar
Schwarzer, R. A. and Sukkau, J. (2003) Automated evaluation of Kikuehi patterns by means of Radon and fast Fourier transformation, and verification by an artificial neural network. Advanced Engineering Materials, 5, 601–606.CrossRefGoogle Scholar
Sevillano, J. G., García-Rosales, C., Echeberria, J. J. and Zubillaga, Y. C. (2000) Structure and crystallographic texture of a metallic meteorite of octahedrite type (Gibeon). Boletin Sociedad Española de Ceramicay Vidrio, 39, 313–318.CrossRefGoogle Scholar
Skála, R. and Císařová, I. (2005) Crystal structure of meteoritic schreibersites: Determination of absolute structure. Physics and Chemistry of Minerals, 31, 721–732.CrossRefGoogle Scholar
Skála, R. and Drábek, M. (2000) Variation of unit-cell dimensions of experimentally synthesized members of Fe3P-Ni3P solid solution (abstract # 1564). 31st Lunar and Planetary Science Conference, CD-ROM.Google Scholar
Zipfel, J., Kim, Y. and Marti, K. (1995) Nitrogen isotopic disequilibrium in the Cape York IIIA iron. Meteoritics, 30, 606.Google Scholar
Zucolotto, M. E. and Pinto, A. L. (2000) Electron back-scattered diffraction studies of the Barbacena meteorite. Meteoritics and Planetary Science, 35, supplement, p. A180 (abstract).Google Scholar
Zucolotto, M. E. and Pinto, A. L. (2001) A metallo-graphic and EBSD study of the Maria Da Fé iron. Meteoritics and Planetary Science, 36, supplement, p. A234 (abstract).Google Scholar