Other
Scientific paper
Aug 1976
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976orli....7..239s&link_type=abstract
Origins of Life, Volume 7, Issue 3, pp.239-257
Other
Scientific paper
Drill core samples of 42 Precambrian sedimentary, igneous, and metamorphic rocks were analyzed by heating under partial vacuum at 100°C and at 400°C to release hydrocarbons and other volatile products. The core samples yielded methane in amounts ranging from traces to 3 microliters per gram, but averaged much less. By way of comparison, samples of Middle Devonian Marcellus black shale, from Pennsylvania, yielded methane in amounts up to 7ul/g. Other straight chain hydrocarbons up to C11 were found in the volatile products, especially those obtained at 400°C, and benzene was a common product, also mainly in the 400°C experiments. Carbon dioxide and nitrogen appear to form a large part of the nonhydrocarbon volatiles in at least some of the samples. Spectral data indicate that the straight chain pyrolysis products of the Precambrian rocks are mainly alkenes, whereas those of the Devonian rocks, referred to above, are a mixture of alkanes and alkenes. Alkanes were however, obtained from several algae-bearing Middle Precambrian argillites. Available evidence indicates, although not conclusively, that the alkenes were contained in the rock rather than being produced from alkanes during pyrolysis. The writers believe that surface contamination in most of the drill cores was minimal owing to the low permeability of the rocks studied, and that contamination by drilling was also minimal. There is a reasonable possibility that the volatiles, if not formed from kerogen residues by the pyrolysis experiments, are in part juvenile igneous gases or are substances that were distilled out of the deeperlying rocks during intervals of folding and metamorphism, and subsequently accumulated at higher levels.
Baysinger J.
Bratt J. M.
Swain F. M.
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