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Keywords:

  • carbon isotope;
  • free-gas;
  • hydrocarbons;
  • in situ fluid;
  • microbial origin;
  • Sagara Drilling Program;
  • Sagara oil field;
  • thermogenic origin

Abstract  We collected free-gas and in situ fluid samples up to a depth of 200.6 m from the Sagara oil field, central Japan (34°44′N, 138°15′E), during the Sagara Drilling Program (SDP) and measured the concentrations and stable carbon isotopic compositions of CH4 and C2H6 in the samples. A combination of the CH4/C2H6 ratios with the carbon isotope ratios of methane indicates that the hydrocarbon gases are predominantly of thermogenic origin at all depths. The isotope signature of hydrocarbon gases of δ13inline image < δ13inline image suggests that these gases in the Sagara oil field are not generated by polymerization, but by the decomposition of organic materials.