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Zhao Changyi, Cheng Kerning, Wang Feiyu. Analyses of the Macerals Contributing Mainly to Hydrocarbons Derived from Coals of the TurpairHami Basin[J]. Acta Sedimentologica Sinica, 1997, 15(2): 95-99.
Citation: Zhao Changyi, Cheng Kerning, Wang Feiyu. Analyses of the Macerals Contributing Mainly to Hydrocarbons Derived from Coals of the TurpairHami Basin[J]. Acta Sedimentologica Sinica, 1997, 15(2): 95-99.

Analyses of the Macerals Contributing Mainly to Hydrocarbons Derived from Coals of the TurpairHami Basin

  • Received Date: 1996-10-12
  • Publish Date: 1997-04-10
  • The Turpan-Hami basin is a typical basin in which hydrocarbons are derived from coalg and main source rocks are coalwith coaly organic matters in the Lower-Middle Jurassic.The analysis of organic petrology showed that the composition ofmaceraLs is of characteristic of the high content of groundmass maceraLs(such as desmocnllinite, macrinite),small individu-als of sporinite and alginite and higher contents of transition macerals(such as vitrinite inertinite desmoc;olHnite and bitu-minite).By mean of nucroscopy, laser microscopy and transmitting electronic microscopy(TEM),it was shown that themain oilg-generating maceraLs are desmocollinite under microscopic observation. Liptodetrinite,。utinite, suberinite and spori-nite have important contributions to thehydro carbon from coal; Under TEM the main oil generating mac}ral is the submi-croliptinite attered in desmoconite and macrinite and it is originated from degraded materials of bacteria. The high con-tent of desmoc collinite in coal remedies its lower hydrocarbon generation potential per unit The cause of hydrogen ric;hnessindesmoc;ollinite attributes to strong degradation and reworking of bacteria to it in the biocthemical stage.
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    2 Powell T G et al, Petroleum sourcz rock assessment in non-marine sequenczs pyrolysis and petrogmphic analysis of Aus-tralian coals and conaceous shales.Org. Geochem. 1991, 17(3): 375-394.

    3 Taylor G H et al, New lightin the origin of Cooper basin oil,A E,A Journal, 1988,30?r 309.

    4 王飞宇等.煤和烃源岩镜质体中超微类脂体检出及意义科学通报.1993, 38(2): 151-154.

    5 Khomsani K G et al, Geological and ratory evidence forearly generation of large amounts of lidtid hydrocarbons fromsuberinite and subereous Components. Org. Geochen 1991, 17(6): 349-86

    6 赵长毅.煤及源岩的有机成分激光诱导荧光研究方法、机理及应用.中国矿业人学北京研究生部博士论文.1991.

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  • Received:  1996-10-12
  • Published:  1997-04-10

Analyses of the Macerals Contributing Mainly to Hydrocarbons Derived from Coals of the TurpairHami Basin

Abstract: The Turpan-Hami basin is a typical basin in which hydrocarbons are derived from coalg and main source rocks are coalwith coaly organic matters in the Lower-Middle Jurassic.The analysis of organic petrology showed that the composition ofmaceraLs is of characteristic of the high content of groundmass maceraLs(such as desmocnllinite, macrinite),small individu-als of sporinite and alginite and higher contents of transition macerals(such as vitrinite inertinite desmoc;olHnite and bitu-minite).By mean of nucroscopy, laser microscopy and transmitting electronic microscopy(TEM),it was shown that themain oilg-generating maceraLs are desmocollinite under microscopic observation. Liptodetrinite,。utinite, suberinite and spori-nite have important contributions to thehydro carbon from coal; Under TEM the main oil generating mac}ral is the submi-croliptinite attered in desmoconite and macrinite and it is originated from degraded materials of bacteria. The high con-tent of desmoc collinite in coal remedies its lower hydrocarbon generation potential per unit The cause of hydrogen ric;hnessindesmoc;ollinite attributes to strong degradation and reworking of bacteria to it in the biocthemical stage.

Zhao Changyi, Cheng Kerning, Wang Feiyu. Analyses of the Macerals Contributing Mainly to Hydrocarbons Derived from Coals of the TurpairHami Basin[J]. Acta Sedimentologica Sinica, 1997, 15(2): 95-99.
Citation: Zhao Changyi, Cheng Kerning, Wang Feiyu. Analyses of the Macerals Contributing Mainly to Hydrocarbons Derived from Coals of the TurpairHami Basin[J]. Acta Sedimentologica Sinica, 1997, 15(2): 95-99.
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