Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
Electron Microprobe Analysis of Oxygen in an Iron Meteorite
J. F. Lovering 1 and
C. A. Andersen 2
1 Department of Geophysics, Australian National University, Canberra 2 Hasler Research Center, Applied Research Laboratories, Inc., Goleta, California
A quantitative analysis of oxygen in the iron-nickel matrixof the Santa Catherina iron meteorite has been accomplishedby using an electron microprobe with dispersive x-ray opticsand by applying theoretically calculated corrections to theobserved intensity ratios. Microvolume analyses and two-dimensionalscanning images in OK, FeL, and NiL x-radiation show that thehigh nickel phase of the meteorite has been oxidized while thelow nickel phase has remained unoxidized.