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CHEN Jian fa, XU Yong chang, HUANG Di fan. Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)[J]. Acta Sedimentologica Sinica, 2000, 18(4): 606-610.
Citation: CHEN Jian fa, XU Yong chang, HUANG Di fan. Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)[J]. Acta Sedimentologica Sinica, 2000, 18(4): 606-610.

Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)

  • Received Date: 1999-07-04
  • Rev Recd Date: 2000-05-29
  • Publish Date: 2000-08-10
  • Tarim Basin, located in the northwest China, is one of the largest basins in the world, which has not been well explored. In recent years the large scale of petroleum exploration in the basin has led to the discovery of a series of oil and gas fields, with an approximate 1∶1 ratio of oil to gas resource. This means that the natural gas resource is very important for the hydrocarbon resource in the Tarim basin. In this basin most of the discovered gases are condensate associated gas and oil associated gas. It is show by chemical components analysis that the content of hydrocarbon of the natural gases from this basin is mostly higher than 65%. The content of CO2 is mostly less than 5%. The content of N2 is mostly less than 10% and the N2 in some gases reaches 25% to 35%. The C 1/C 2+ ratios of gases from Tabei area show a generally decreasing trend from east to west.The content of N 2 in gases shows generally Qincreasing trend from east to west.The carbon isotopic composition of methane becomes gradually lighter from east to west. All these may be responsible to the low palaeozoic source rock,of which maturity is generally becoming lower from east to west.
  • [1] 童晓光.塔里木盆地的地质结构和油气聚集[A].见:童晓光、粱狄刚主编,塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社,1992.17~22
    [2] 周清杰,郑建京.塔里木盆地构造分析[M].北京:科学出版社,1990
    [3] Graham S A, Brassell S, Carrroll A R, Xiao X. Characteristics of selected petroleum source rock, Xinjiang Uygur Autonomous region, Northwest China[J]. AAPG. Bulletin, 1990, 74. 4, 496~512
    [4] 粱狄刚,王会祥,塔里木盆地的油源问题[A].见:童晓光,粱狄刚主编,塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社,1992.321~330
    [5] 王社教,王会祥,谢增业,李梅.塔里木盆地三套生油层成熟演化及成烃期的研究[A].见:童晓光,粱狄刚主编,塔里木盆地油气勘探论文集[C].乌鲁木齐:新疆科技卫生出版社,1992.331~342
    [6] Stahl W. Carbon isotope fractionations in natural gases[J]. Nature,1974,251(1): 134~135
    [7] Schoell M. Genetic characterization of natural gases[J]. AAPG Bulletin1983, 67(12):2 225~2 238.
    [8] Whiticar M. A geochemical perspective of natural gas and atnospheric methane[J]. Org. Geochem.,1990, 16 (1~3):531~547
    [9] 戴金星.各类烷烃气的鉴别[J].中国科学,1992,22(2):187~193l
    [10] 徐永昌等.天然气成因理论及应用[M].北京:科学出版社,1994
    [11] Stahl W. Carbon and nitrogen isotopes in hydrocarbon research and exploration[J]. Chemical Geology, 1977, 20, 121 ~ 149.
    [12] 陈践发,李春园,应光国,沈平.煤型气烃类组分的稳定碳、氢同位素组成研究[J].沉积学报,1995,13(2):59~69
    [13] Galimov E. Source and mechanisms of formation of gasseous hydrocarbons in sedimentary rock[J]. Chemical Geology, 1988,1/3:77~95
    [14] Fuex A N. The use of stable carbon isotopes in hydrocarbon exploration[J]. J. Geochem. Explor.,1977,7:155~188
    [15] James A T. Correlation of natural gas by use of carbon isotopic distribution between hydrocarbon components [J]. Am. Assoc. Geol.Bull.,1983, 67:1176~1191
    [16] Berner U, Faber E. Maturity related mixing model for methane, ethane and propane, based on carbon isotopes [J] Org. Geochem.1988,13:67~72
    [17] Schoell M. The hydrogen and carbon isotopic composition of methane from natural gases of various origins[J]. Geochemical et Cosmochimica Acta, 1980,44:649~662
    [18] Sundberg K R, Bennett C R. Carbon isotope palleothermometry of natural gas[A]. In:Bjoroy M, Albrecht P, Comford C. et al., eds. Advances in organic geochemistry - 1981 [C]. Chichester, England,John Wiley and Son, 1983.769~774
    [19] Faber E. Zur Isotopengeochemie gasformiger Kohlenwasserstoffe[J]. Erdol, Kohle, 1987,103:210~218
    [20] Jenden P D, Drazan D J, Kaplan I R. Mixing of therrmogenic natural gases in Northern Appalachian basin [J]. Am. Assoc. Geol. Bull. 1993,77:980~998
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  • Received:  1999-07-04
  • Revised:  2000-05-29
  • Published:  2000-08-10

Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)

Abstract: Tarim Basin, located in the northwest China, is one of the largest basins in the world, which has not been well explored. In recent years the large scale of petroleum exploration in the basin has led to the discovery of a series of oil and gas fields, with an approximate 1∶1 ratio of oil to gas resource. This means that the natural gas resource is very important for the hydrocarbon resource in the Tarim basin. In this basin most of the discovered gases are condensate associated gas and oil associated gas. It is show by chemical components analysis that the content of hydrocarbon of the natural gases from this basin is mostly higher than 65%. The content of CO2 is mostly less than 5%. The content of N2 is mostly less than 10% and the N2 in some gases reaches 25% to 35%. The C 1/C 2+ ratios of gases from Tabei area show a generally decreasing trend from east to west.The content of N 2 in gases shows generally Qincreasing trend from east to west.The carbon isotopic composition of methane becomes gradually lighter from east to west. All these may be responsible to the low palaeozoic source rock,of which maturity is generally becoming lower from east to west.

CHEN Jian fa, XU Yong chang, HUANG Di fan. Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)[J]. Acta Sedimentologica Sinica, 2000, 18(4): 606-610.
Citation: CHEN Jian fa, XU Yong chang, HUANG Di fan. Geochemical Characteristics and Origin of Natural Gas in the Eastern Tarim Basin(I)[J]. Acta Sedimentologica Sinica, 2000, 18(4): 606-610.
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