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Carbon isotopic compositions of 1,2,3,4-tetramethylbenzene in marine oil asphaltenes from the Tarim Basin:Evidence for the source formed in a strongly reducing environment被引量:5
2008年
Although 1-alkyl-2,3,6-trimethylbenzenes and a high relative amount of 1,2,3,4-tetramethylbenzene have been detected in marine oils and oil asphaltenes from Tabei uplift in the Tarim Basin, their bio-logical sources are not determined. This paper deals with the molecular characteristics of typical ma-rine oil asphaltenes from Tabei and Tazhong uplift in the Tarim Basin and the stable carbon isotopic signatures of individual compounds in the pyrolysates of these asphaltenes using flash pyrolysis-gas chromatograph-mass spectrometer (PY-GC-MS) and gas chromatograph-stable isotope ratio mass spectrometer (GC-C-IRMS), respectively. Relatively abundant 1,2,3,4-tetramethylbenzene is detected in the pyrolysates of these marine oil asphaltenes from the Tarim Basin. δ 13C values of 1,2,3,4-tetrame-thylbenzene in the pyrolysates of oil asphaltenes vary from-19.6‰ to-24.0‰, while those of n-alkanes in the pyrolysates show a range from-33.2‰ to-35.1‰. The 1,2,3,4-tetramethylbenzene in the pyro-lysates of oil asphaltenes proves to be significantly enriched in 13C relative to n-alkanes in the pyro-lysates and oil asphaltenes by 10.8‰―15.2‰ and 8.4‰―13.4‰, respectively. This result indicates a contribution from photosynthetic green sulfur bacteria Chlorobiaceae to relatively abundant 1,2,3,4-tetramethylbenzene in marine oil asphaltenes from the Tarim Basin. Hence, it can be speculated that the source of most marine oil asphaltenes from the Tarim Basin was formed in a strongly reducing water body enriched in H2S under euxinic conditions.
JIA WangLuPENG PingAnXIAO ZhongYao
关键词:ASPHALTENESMARINETARIMISOTOPIC
塔里木盆地典型海相原油沥青质中1,2,3,4-四甲基苯的碳同位素组成--母源形成于强还原环境的证据被引量:5
2008年
尽管已经有塔里木盆地塔北地区海相原油沥青质中以及原油中1,2,3,4-四甲基苯与1-烷基-2,3,6-三甲基苯系列化合物检出的报道,但其来源仍然未得到证实.分别利用瞬间热解-气相色谱-质谱(PY-GC-MS)与气相色谱-同位素比值质谱联用技术(GC-C-IRMS)研究了塔里木盆地塔北与塔中地区典型海相原油沥青质的热解产物组成与热解产物中单个化合物的碳同位素组成.结果表明,原油沥青质的热解产物中普遍检出了高含量的1,2,3,4-四甲基苯.热解产物中1,2,3,4-四甲基苯的δ13C值在-19.6‰~-24.0‰之间,正构烷烃的δ13C范围在-33.2‰~-35.1‰之间.1,2,3,4-四甲基苯相对于正构烷烃以及原油沥青质显著富集13C(分别达10.8‰~15.2‰与8.4‰~13.4‰),证明塔里木盆地海相原油沥青质热解产物中检出的丰富的1,2,3,4-四甲基苯来源于营光合作用的绿硫细菌(Chlorobiaceae).由此可推测塔里木盆地多数海相原油沥青质的母源应形成于静水条件下H2S充溢的强还原环境.
贾望鲁彭平安肖中尧
关键词:沥青质塔里木盆地碳同位素组成
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