Physics
Scientific paper
Oct 1964
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1964gecoa..28.1729r&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 28, Issue 10-11, pp.1729-1743
Physics
5
Scientific paper
The fluorine content of stony meteorites was measured by F 18 produced by an activation technique. Different classes of chondrites, enstatite, `ordinary' and pigeonite-Wiik Class III, contain amounts of fluorine, 238, 121 and 66 ppm respectively that in a sense reflect their state of oxidation. In general, the fluorine concentration within a class of stone meteorites is fairly constant. The enstatite chondrite, Hvittis, seems to be an exception. Two Ca-rich and one Ca-poor achondrites contain about 63 and 11 ppm F, respectively. An atomic abundance of 1.6 × 10 3 atoms F/10 6 atoms Si postulated by and (1956) was confirmed.
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