Gao Fuhong, Gao Hongmei, Fan Fu. GEOCHEMICAL CHARACTERISTICS OF BIOMARKERS EXTRACTED FROM THE LOWER CRETACEOUS COAL MEASURES ROCKS IN JIXI BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(2): 188-191. doi: 10.11781/sysydz200702188
Citation: Gao Fuhong, Gao Hongmei, Fan Fu. GEOCHEMICAL CHARACTERISTICS OF BIOMARKERS EXTRACTED FROM THE LOWER CRETACEOUS COAL MEASURES ROCKS IN JIXI BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(2): 188-191. doi: 10.11781/sysydz200702188

GEOCHEMICAL CHARACTERISTICS OF BIOMARKERS EXTRACTED FROM THE LOWER CRETACEOUS COAL MEASURES ROCKS IN JIXI BASIN

doi: 10.11781/sysydz200702188
  • Received Date: 2006-05-25
  • Rev Recd Date: 2007-01-31
  • Publish Date: 2007-03-28
  • By the Gas chromatography and the Gas chromatography-mass spectrogram analysis,the biomarkers in the Lower Cretaceous mud rocks and coals of coal measures from Jixi Basin were studied.The results indicate that n-alkanes in mud rocks show front single-peak type,with the main peak carbons to be C16 or C18.The ratio of Pr/Ph is 2.86~11.22,Pr/n C17 is larger than 1.The n-alkanes in coals show rear single-peak type,with the main peak carbons to be C22 or C23.The ratios of Pr/Ph and Pr/n C17 are 2.86~11.22 and 2.1~3.33 respectively.The values of the OEP and CPI in both mud rocks and coals concentrale on 1.0.The thermal evolution has reached maturation stage.The biomarkers in mud rocks show that the ratio of tricycle terpane plus tetracyclic terpane to C30H is 2.37~3.62.The C3122S/22(S+R),Ts/Tm and G/C30H are 0.57~0.61,0.47~0.81 and 0.11~0.34 respectively.The ααα20R homosteranes in mud rocks appears to be in asymmetrical "V"distribution.The analytic result of the biomarkers show the mud rocks coming mainly from aquatic organisms and depositing in reducing environment with more saline water,which is better for preservation and transformation of organics.The biomarkers in coals show that the ratio of tricycle terpane plus tetracyclic terpane to C30H is lower than that in mud rocks.The ratio of C3122S/22(S+R) is about 0.6,the Ts/Tm and G/C30H are very low.The ααα20R homosteranes of coals appear to be in inverted "L" distribution.The coals are mainly from higher plants,and deposit in oxidizing environment.

     

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