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Carbon isotope geochemistry of natural gases from the Green Tuff basin, Japan

Journal Article · · Geochimica et Cosmochimica Acta; (United States)
 [1]
  1. Geological Survey of Japan, Ibaraki (Japan)

Carbon isotopic analyses of C{sub 1}-C{sub 4} hydrocarbons were carried out to investigate the origin and formation mechanism of natural gases commercially produced from volcanic rocks as well as sedimentary rocks in the Green Tuff basin of Northeast Japan, whose high {sup 3}He/{sup 4}He ratios have suggested a possible magmatic origin. {delta}{sup 13}C (PDB) values of methane, ethane, propane, and n-butane range from {minus}54.4 to {minus}33.3{per thousand}, from {minus}32.5 to {minus}20.9{per thousand}, from {minus}27.7 to{minus}20.6{per thousand}, and from {minus}25.3 to {minus}20.5{per thousand}, respectively, all of which fall within the ranges of published data of worldwide gases of biogenie origin. Most samples show the isotope distribution pattern wherein the {delta}{sup 13}C values become less negative with increasing molecular weight of the hydrocarbons, suggesting that the C{sub 2{sup +}} hydrocarbons were not derived by methane polymerization. The {delta}{sup 13}C values of C{sub 2}-C{sub 4} hydrocarbons are explained by thermogenic breakdown of organic matter, whereas the {delta}{sup 13}C values of methane are more or less lower than those expected from the same origin. These results indicate that the gases from the Green Tuff Basin consist of thermogenic hydrocarbons plus variable amounts of isotopically lighter microbial methane. Significant contributions of abiogenic methane, which would be isotopically heavier than the thermogenic methane, are not plausible for the gases.

OSTI ID:
6082648
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Journal Name: Geochimica et Cosmochimica Acta; (United States) Vol. 55:5; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English