2017 Vol. 23, No. 4
Article Contents

DONG Hui, WANG Zhihai, DONG Min, LI Hong, WEI Xiaoyan, LIANG Jiwei. APPLICATION OF LASER RAMAN SPECTROSCOPY IN THE STUDY OF ORGANIC INCLUSIONS: A CASE STUDY ON OIL AND GAS INCLUSIONS IN THE 8th MEMBER OF THE SHIHEZI FORMATION IN WESTERN SULIGE GASFIELD[J]. Journal of Geomechanics, 2017, 23(4): 594-601.
Citation: DONG Hui, WANG Zhihai, DONG Min, LI Hong, WEI Xiaoyan, LIANG Jiwei. APPLICATION OF LASER RAMAN SPECTROSCOPY IN THE STUDY OF ORGANIC INCLUSIONS: A CASE STUDY ON OIL AND GAS INCLUSIONS IN THE 8th MEMBER OF THE SHIHEZI FORMATION IN WESTERN SULIGE GASFIELD[J]. Journal of Geomechanics, 2017, 23(4): 594-601.

APPLICATION OF LASER RAMAN SPECTROSCOPY IN THE STUDY OF ORGANIC INCLUSIONS: A CASE STUDY ON OIL AND GAS INCLUSIONS IN THE 8th MEMBER OF THE SHIHEZI FORMATION IN WESTERN SULIGE GASFIELD

  • Based on the application of laser raman microprobe analysis in situ technique, the nature of oil and gas inclusions in the 8th member of the Shihezi formation in western Sulige gas field was identified. The composition and relative molar fraction of phaseⅡhydrocarbon-bearing organic inclusions in the healing fracture of the quartz grain surface and in the secondary enlargement margin were determined. The results show that the early-stage inclusions mainly are gas-liquid two-phase organic inclusions containing gaseous hydrocarbon and brine gaseous hydrocarbon, and the late-stage inclusions are gas-liquid two-phase organic inclusions containing gaseous hydrocarbon; The gas phase is dominated by gases such as CO2, CH4 and N2, and the CO, H2S, H2, C2H2, C2H4, C2H6, C4H6, H2O and CO2are dissolved in it; the liquid phase mainly is consist of H2O and CO2, and also contains a very small amount of anion SO42- and CO32-(less than 0.03 mol/L). The research makes clear that the early-stage organic inclusions contain large amounts of CO2, H2O and a small amount of inorganic gas of low carbon alkane. It indicates that the early maturity of organic matter was in immature-low mature stage. Although natural gas is generated, the migration is limited in scale. The organic inclusions are few and far between. It reflects the replacement of formation water by natural gas entering reservoir. The late-stage organic inclusions are the opposite. The content of hydrocarbons and N2 are higher, but the content of CO2, inorganic gas and H2O are lower. It represents the characteristics of the peak of oil and gas formation and large-scale oil and gas accumulation. It provides a scientific basis for the thermal evolution of organic matter, the generation and migration of oil and gas, and the division of oil and gas accumulation stages.

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