Results of measurements of fluorinated compounds in gasses extracted from i
gneous and metamorphic rocks are reported. A new extraction method analogou
s to a pepper mill for geological samples is described. It permits extracti
on at low temperatures and ensures a rapid transfer of extracted gases from
active surfaces to cryogenic pre-concentration loop. Values for CF4, CF3Cl
, CF2Cl2, CFCl3, CHF3, SF6 and NF3 in fluorites, granites, basalts and othe
r igneous and metamorphic rocks are reported. It is proposed that trifluoro
acetic acid (TFA) that was recently discovered in various environmental arc
hives could also origin from similar geogenic sources.