Computer Science
Scientific paper
Mar 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993lpi....24..987m&link_type=abstract
In Lunar and Planetary Inst., Twenty-Fourth Lunar and Planetary Science Conference. Part 2: G-M p 987-988 (SEE N94-16173 03-91)
Computer Science
1
Achondrites, Crystallography, Grain Size, Meteoritic Composition, Mineralogy, Crystals, Olivine, X Ray Diffraction
Scientific paper
Mineralogy of kirschsteinite exsolution in olivine from Antarctic meteorite LEW86010 has been studied by single crustal X-ray diffraction technique. The LEW86010 olivine crystals have exsolution lamellae of kirschteinite about 15 microns wide. Determination of crystallographic orientation of exsolved kirschsteinite in an olivine grain has been made. Weak reflections of exsolved kirschsteinite share common crystallographic orientation with the host olivine. The cell dimensions of the exsolved phase (a - 4.87 plus or minus 0.05A, b - 11.14 plus or minus 0.10A, c - 6.36 plus or minus 0.05A) and intensities were in well accord with those of kirschsteinite previously reported. Oriented section perpendicular to the a axis shows exsolution lamellae in two directions parallel to (031) and (031). The lamellae are up to 10 microns in width and spacings between them are usually 50-100 microns.
McKay Gordon
Mikouchi Takashi
Miyamoto Masamichi
Mori Hiroshi
Takeda Hiroshi
No associations
LandOfFree
Exsolved kirschsteinite in angrite LEW86010 olivine does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Exsolved kirschsteinite in angrite LEW86010 olivine, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Exsolved kirschsteinite in angrite LEW86010 olivine will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1449934