Mineralogy of artificially heated carbonaceous chondrites

Details Mineralogy of artificially heated carbonaceous chondrites Mineralogy of artificially heated carbonaceous chondrites

Mar 1994

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994lpi....25.1567z&link_type=abstract

In Lunar and Planetary Inst., The Twenty-Fifth Lunar and Planetary Science Conference. Part 3: P-Z p 1567-1568 (SEE N94-35448 11

Physics

3

Carbonaceous Chondrites, Heating, Mineralogy, Phase Transformations, Temperature Effects, Crystallization, Electron Probes, Hydrogen, Olivine, Serpentine, X Ray Diffraction

Scientific paper

We have examined suites of heated Murchison (CM2) and Allende (CV3)
samples heated in the range 400-1200 C, in a H2 atmosphere with a
pressure of 105 bar for periods of 1 to 4 weeks. We used a
combination of X-ray diffraction, electron microprobe and TEM analyses
to determine the mineralogy of these samples.

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