Mathematics – Logic
Scientific paper
Mar 1974
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1974gecoa..38..471l&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 38, Issue 3, pp.471-477
Mathematics
Logic
5
Scientific paper
Equilibration temperatures for enstatite chondrites are calculated using a method suggested by (1968). The temperatures range from 640° to 840°C. The method yields temperatures which, in principle, are correct on a relative scale but the absolute error may be a large as 150°. There is a good correlation between the calculated temperatures and petrologic type as well as other mineralogic characteristics and bulk composition. Partial pressures of sulfur and oxygen at the time of equilibration were: pS 2 ~ 10 -8 -10 -12 atm and pO 2 ~ 10 -28 -10 -37 .
Buseck Peter R.
Larimer John W.
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