Advanced Search
Volume 22 Issue 4
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2000  >  22(4): 297-301
HUANG Hai-ping. FORMING MECHANISM OF HYDROCARBON POOLS IN TAHE OILFIELD OF THE NORTHERN TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2000, 22(4): 297-301. doi: 10.11781/sysydz200004297
Citation: HUANG Hai-ping. FORMING MECHANISM OF HYDROCARBON POOLS IN TAHE OILFIELD OF THE NORTHERN TARIM BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2000, 22(4): 297-301. doi: 10.11781/sysydz200004297
shu

FORMING MECHANISM OF HYDROCARBON POOLS IN TAHE OILFIELD OF THE NORTHERN TARIM BASIN

doi: 10.11781/sysydz200004297

  • Department of Energy Resource Geology, China University of Geosciences, Beijing 100083, China

  • Received Date: 2000-02-14
  • Publish Date: 2000-10-25
    Abstract
  • High temperature GC analysis of high molecular weight hydrocarbons (HMWHCs) was performed on marginal mature source rock extractions from the Shahejie Formation, Damintun Depression, whose oil is particularly rich in wax. Organic composition and depositional environment are the main control factors for the formation of HMWHCs. The main maceral components in organic-rich samples (TOC>3.0%) are liptinite and exinite, deposited in relatively reduced environment. They contain high amount of waxes but dominated by macrocrystalline ones (centred at C29). Those organic-lean samples (TOC<2.0%) are dominated by vitrinite, deposited in a slightly oxidized environment. They contain lower amount of waxes but relatively rich in microcrystalline components. Besides normal alkanes, high amounts of branched/cyclic hydrocarbons have been detected in the region above C50.

     

    • FullText(HTML)
  • loading
    • References(17)
  • [1]
    Hedberg H D. Significance of high wax oils with respect to genesis of petroleum[J]. Am Assoc Petrol Geol Bull,1968,52:736-750.
    [2]
    Tissot B P, Welte D H. Petroleum formation and occurrence[M], 2nd Ed. Springer-Verlag, 1984.
    [3]
    Tegelaar E W, Matthezing R M, Jansen J B H, Horsfield B, de Leeuw J W. Possible origin of n-alkanes in high wax crude oils[J]. Nature, 1989,342:529-531.
    [4]
    Del Rio J C, Philp R P. Nature and geochemistry of high weight hydrocarbons (above C40) in oils and solid bitumens[J]. Org Geochem,1992,18(4):541-553.
    [5]
    Del Rio J C, Philp R P. Field ionization mass spectrometric study of high molecular weight hydrocarbons in a crude oil and a solid bitumen[J]. Org. Geochem.,1999, 30:279-286.
    [6]
    Carlson R M K, Teerman S C, Moldowan J M, Jacobson S R, Chan E I, Dorrough K S, Seetoo W C, Mertani B. High temperature gas chromatography of high wax oils[A]. Indonesian Petroleum Association, 22nd Annual Convention Proceedings[C]. Jakarta, Indonesian, 1993. 483-507.
    [7]
    Musser B, Kilpatrick P K. Molecular characterization of wax isolated from a variety of crude oils[J]. Energy & Fuels, 1998,12:715-725.
    [8]
    Thanh N X, Hsieh M, Philp R P. Waxes and asphaltenes in crude oils[J]. Org Geochem, 1999,30: 119-132.
    [9]
    郑容植,王桂珍.大民屯凹陷高凝油低凝油特征及其分布规律[J],石油实验地质,1988,10(3): 256-267.
    [10]
    葛泰生,陈义贤. 中国石油地质志(卷三)——辽河油田[M]. 北京:石油工业出版社,1993.
    [11]
    Tong X, Huang Z. Buried-hill discoveries of the Damintun Depression in North China[J]. Am Assoc Petrol Geol Bull,1991, 75:780-794.
    [12]
    Huang Y, Geng A, Fu J, Sheng G, Zhao B, Cheng Y, Li M. The inverstigation of characteristics of biomarker assemblages and their precursors in Damintun ultra-high wax oils and related source rocks[J]. Org Geochem, 1992,9:29-39.
    [13]
    Didyk B M, Simoneit B R T, Brassel S C, Eglinton G. Organic geochemical indicators of paleoenvironmental conditions of sedimentation[J]. Nature,1978,272:216-222.
    [14]
    Mello M R, Maxwell J R. Organic geochemical and biological marker characterization of source rocks and oils from lacustrine environments in the Brazilian Continental Margin[A]. Katz B J Lacustrine Basin Exploration[C]. AAPG Memoir 50.1990.77-97.
    [15]
    Philp P R. Geochemical characteristics of oils derived predominantly from terrigenous source materials[A]. Scott A C, Fleet A J. Coal and coal-bearing strata as oil-prone source rocks?[C]. Geological Society Special Publication, London, 1990.71-91.
    [16]
    Fu J, Sheng G. Biological marker composition of typical source rocks and related crude oils of terrestrial origin in the People's Republic of China: a review[J]. Appl Geochem, 1989,4:13-22.
    [17]
    Hughes W B, Holba A G, Dzou L I P. The ratios of dibenzothiophene to phenanthrene and pristane to phytane as indicators of depositioal environment and lithology of petroleum source rocks[J]. Geochimica et Cosmochimica Acta,1995,59: 3581-3598.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (769) PDF downloads(425) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return