Oil & Gas Geology ›› 1980, Vol. 1 ›› Issue (1): 47-55.doi: 10.11743/ogg19800106

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EVOLUTION OF KEROGEN IN THE OIL-GAS FORMATION IN THE PALAEOZOIC SEDIMENTS OF SHAANXI-GANSU-NINGXIA BASIN

Fan Pu1, Shen Ping1, Rong Guanghua1, Wang Hongyong1, Ye Jisun2   

  1. 1. Lanzhou Institute of Geology, Academia Sinica;
    2. Guiyang Institute of Geochemistry, Academia Sinica
  • Online:1980-06-25 Published:2012-01-16

Abstract:

The characteristics of pyrolysis(P-FID),thermogravimetric analysis (TGA),infrared spectrums(IR),elements composition and carbon isotope ratios of kerogen in the Palaeozoic rocks of the Shaanxi-Gansu-Ningxia Basin have been investigated,and the types of kerogen in vari-ous sequences have been described in this paper.The main types of ke-rogen favourable to oil-gas formation in this basin are sapropel(O2)and mixed humus and sapropel(C2b,C3t),because of their high con-tents of C degradation hydrocarbons,It is suggested that,with the grade of metamorphism getting higher,the H/C(atomic ratio) and O/C(atomic ratio)of kerogen tend to de-crease,the H/C(atomic ratio)of asphaltene and the fractionation ofδC13 to increase.