Oil & Gas Geology ›› 1980, Vol. 1 ›› Issue (1): 47-55.doi: 10.11743/ogg19800106
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Fan Pu1, Shen Ping1, Rong Guanghua1, Wang Hongyong1, Ye Jisun2
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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.
Fan Pu, Shen Ping, Rong Guanghua, Wang Hongyong, Ye Jisun. EVOLUTION OF KEROGEN IN THE OIL-GAS FORMATION IN THE PALAEOZOIC SEDIMENTS OF SHAANXI-GANSU-NINGXIA BASIN[J]. Oil & Gas Geology, 1980, 1(1): 47-55.
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URL: http://ogg.pepris.com/EN/10.11743/ogg19800106
http://ogg.pepris.com/EN/Y1980/V1/I1/47