Hostname: page-component-848d4c4894-p2v8j Total loading time: 0.001 Render date: 2024-05-15T07:01:35.826Z Has data issue: false hasContentIssue false

High-Resolution Electron Microscopy of Olivine-Magnetite Interfaces.

Published online by Cambridge University Press:  25 February 2011

Stuart Mckernan
Affiliation:
Department, of Chemical Engineering and Materials Science, University of Minnesota, Minneapolis, MN 55455.
C. Barry Carter
Affiliation:
Department, of Chemical Engineering and Materials Science, University of Minnesota, Minneapolis, MN 55455.
Get access

Abstract

In the oxidation of iron-rich olivine (Mg,Fe)2SiO4 at elevated temperatures interfaces between olivine and the magnetite spinel (Fe3O4) are formed. The orientation relation between these structures is such that the planar spacing for the principal low index planes are very closely matched in the two materials. Regions of different contrast are observed in the olivine up to 5–10 nm from the interface. It is proposed that this contrast is due to enhanced iron concentration in this region caused by the strain field around the magnetite precipitates.

Type
Research Article
Copyright
Copyright © Materials Research Society 1993

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

REFERENCES

Champness, P. E., Mineral. Mag. 37, 790 (1970).CrossRefGoogle Scholar
2. Kohlstedt, D. L. and Vander Sande, L. B., Contrib. Mineral. Petrol. 53, 13 (1975).CrossRefGoogle Scholar
3. Carter, C. B., Ber. Bunsenges. Phys. Chem. 90, 643 (1986).CrossRefGoogle Scholar
4. McKernan, S., Rasmussen, D.R. and Carter, C.B., Proc. Mat. Res. Symp. Proc. 139, p. 309, (1989)CrossRefGoogle Scholar