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LI Jing-gui, ZHENG Jian-jing, LIU Wen-hui, CHEN Guo-jun, MENG Zi-fang. Dibenzothiophene Series from the Carbonate Rocks and Their Crude Oils in Tabei and Tazhong Areas,Tarim basin[J]. Acta Sedimentologica Sinica, 2004, 22(2): 348-353.
Citation: LI Jing-gui, ZHENG Jian-jing, LIU Wen-hui, CHEN Guo-jun, MENG Zi-fang. Dibenzothiophene Series from the Carbonate Rocks and Their Crude Oils in Tabei and Tazhong Areas,Tarim basin[J]. Acta Sedimentologica Sinica, 2004, 22(2): 348-353.

Dibenzothiophene Series from the Carbonate Rocks and Their Crude Oils in Tabei and Tazhong Areas,Tarim basin

  • Received Date: 2003-04-25
  • Rev Recd Date: 2003-10-23
  • Publish Date: 2004-06-10
  • According to characteristics of compositions and abundances, the dibenzothiophene series of Cambrian and Ordovician carbonate source rocks(marls, muddy limestone and dolomites) from four wells (KN1, LN46, TZ12 and TaCl) in Tabei and Tazhong areas, Tarim basin can be divided into three different types. They are:Ⅰ dibenzothiophene, methyldibenzoth iophene type; Ⅱ dibenzothiophene, methyldibenzothiophene, dimethyldi benzothiophene+trimethylfluorene mixture type; and Ⅲ dibenzothioph ene, methyldibenzothiophene, dimethyldibenzothiophene and trimethyl dibenzothiophene type. The distribution patterns of dibenzothiophene series of eleven marine crude oil samples from Tabei and Tazhong uplifts are, without exception, dibenzothiophene, methyldibenzothiophene, dimethyldibenzothiophene and trimethyldibenzothiophene types, which are very identical to Ⅲ types of above Cambrian and Ordovician marine carbonate source rock samples. Hence, it is inferred that the eight marine crude oil samples from Tabei uplift are thought mainly to possibly derive from Lower Ordovician marine source rocks of Tabei Lunnan area, the three marine crude oil samples from Tazhong uplift possibly from Middle-Upper Ordovician marine source rocks of Tahzhong area.
  • [1] Hanson A D, Zhang S C, Moldowan J M, et al. Molecular organic geo chemistry of the Tarim basin,Northwest China. AAPG Bulletin, 2000, 84(8): 1109~1128
    [2] Cheng J, Fu J, Sheng G, et al. Diamond hydrocarbon ratios:novel maturity indices for highly mature crude oils. Organic Geochemistry,1996, 25(3/4): 179~190
    [3] Zhang S, Moldowan J M, Bian L, et al. Biological and molecualr geochemical evidence for dinoflagellate ancestors in the Upper Sinian-Cambrian. Acta Geologica Sinica, 2000, 74(4):740~747
    [4] Zhang S, Hanson A D, Moldowan J M, et al. Paleozoic oil-source rock correlations in the Tarim basin,NW China. Organic Geochemistry, 2000, 31(4): 273~286
    [5] 黄第藩,赵孟军. 下古生界海相原油之中蜡的成因分析--干酪根PY-GC分析提供的证据. 沉积学报,1996, 14(2):12~19[Huang D, Zhao M. The genesis of marine oils with middle wax from Lower Palaeozoic--evidences obtainined from kerogens PY-GC analysis. Acta Sedimentologica Sinica, 1996, 14(2):12~19]
    [6] Wilhelms A, Telnaes N, Steen A, et al. A quantitative study of aromatic hydrocarbons in a natural maturity shale sequence-the 3-methylphenanthrene/retene ratio,a pragmatic maturity parameter. Organic Geochemistry, 1998, 29(1~3): 97~105
    [7] 刘德汉,史继扬, 郑旭明. 高演化碳酸盐岩的地球化学特征及非常规评价方法的探讨.天然气工业,1994,14(增刊): 62~66[Liu D, Shi J, Zheng X. A discussion on the geochemical characteristics and unconventional evaluation method of high altered carbonate rocks. Natural Gas Industry, 1994, 14(suppl.): 62~66]
    [8] Fan P, Philp R P, Li Z, et al. Geochemical characteristics of aromatic hydrocarbons in crude oils and source rocks from different sedimentary environments. Organic Geochemistry, 1990, 16(1~3): 427~435
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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  • Received:  2003-04-25
  • Revised:  2003-10-23
  • Published:  2004-06-10

Dibenzothiophene Series from the Carbonate Rocks and Their Crude Oils in Tabei and Tazhong Areas,Tarim basin

Abstract: According to characteristics of compositions and abundances, the dibenzothiophene series of Cambrian and Ordovician carbonate source rocks(marls, muddy limestone and dolomites) from four wells (KN1, LN46, TZ12 and TaCl) in Tabei and Tazhong areas, Tarim basin can be divided into three different types. They are:Ⅰ dibenzothiophene, methyldibenzoth iophene type; Ⅱ dibenzothiophene, methyldibenzothiophene, dimethyldi benzothiophene+trimethylfluorene mixture type; and Ⅲ dibenzothioph ene, methyldibenzothiophene, dimethyldibenzothiophene and trimethyl dibenzothiophene type. The distribution patterns of dibenzothiophene series of eleven marine crude oil samples from Tabei and Tazhong uplifts are, without exception, dibenzothiophene, methyldibenzothiophene, dimethyldibenzothiophene and trimethyldibenzothiophene types, which are very identical to Ⅲ types of above Cambrian and Ordovician marine carbonate source rock samples. Hence, it is inferred that the eight marine crude oil samples from Tabei uplift are thought mainly to possibly derive from Lower Ordovician marine source rocks of Tabei Lunnan area, the three marine crude oil samples from Tazhong uplift possibly from Middle-Upper Ordovician marine source rocks of Tahzhong area.

LI Jing-gui, ZHENG Jian-jing, LIU Wen-hui, CHEN Guo-jun, MENG Zi-fang. Dibenzothiophene Series from the Carbonate Rocks and Their Crude Oils in Tabei and Tazhong Areas,Tarim basin[J]. Acta Sedimentologica Sinica, 2004, 22(2): 348-353.
Citation: LI Jing-gui, ZHENG Jian-jing, LIU Wen-hui, CHEN Guo-jun, MENG Zi-fang. Dibenzothiophene Series from the Carbonate Rocks and Their Crude Oils in Tabei and Tazhong Areas,Tarim basin[J]. Acta Sedimentologica Sinica, 2004, 22(2): 348-353.
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