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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2008  >  30(3): 276-280
Li Zhiming, Qin Jianzhong, Xu Xuhui, Liu Wenbin, Shi Weijun, Jiang Hong. THE RELATIONSHIP BETWEEN VITRINITE REFLECTANCE SUPPRESSION AND SOURCE ROCK QUALITY—A CASE STUDY ON SOURCE ROCKS FROM THE DONGYING SAG, BOHAI BAY BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(3): 276-280. doi: 10.11781/sysydz200803276
Citation: Li Zhiming, Qin Jianzhong, Xu Xuhui, Liu Wenbin, Shi Weijun, Jiang Hong. THE RELATIONSHIP BETWEEN VITRINITE REFLECTANCE SUPPRESSION AND SOURCE ROCK QUALITY—A CASE STUDY ON SOURCE ROCKS FROM THE DONGYING SAG, BOHAI BAY BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2008, 30(3): 276-280. doi: 10.11781/sysydz200803276
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THE RELATIONSHIP BETWEEN VITRINITE REFLECTANCE SUPPRESSION AND SOURCE ROCK QUALITY—A CASE STUDY ON SOURCE ROCKS FROM THE DONGYING SAG, BOHAI BAY BASIN

doi: 10.11781/sysydz200803276
  • 1.

    Wuxi Research Institute of Petroleum Geology, RIPEP, SINOPEC, Wuxi, Jiangsu 214151, China

  • 2. Research Institute of Petroleum Exploration and Production, SINOPEC, Beijing 100083, China

  • Received Date: 2007-11-09
  • Rev Recd Date: 2008-05-20
  • Publish Date: 2008-05-28
    Abstract
  • FAMM(fluorescence alteration of multiple macerals) technique is an only effective method for resolving vitrinite reflectance suppression of source rock at present.The FAMM and vitrinite reflectance of various type source rocks are determined in this paper.The relationship between vitrinite reflectance suppression and source rock quality is studied on the basis of measured data and combined with result of predecessors.The studied results show that the levels of vitrinite reflectance suppression are closely related to source rocks quality.The level of vitrinite reflectance suppression is relatively higher in the source rock with better quality.The level of vitrinite reflectance suppression for the source rocks characterized by type Ⅰorganic matter usually ranges from 0.20%～0.35%,average 0.30%;for those characterized by type Ⅱ1 it usually ranges from 0.15%～0.30%,average 0.22%;for those characterized by type Ⅱ2 it usually ranges from 0.10%～0.18%,average 0.15% and for those characterized by type Ⅲ it usually ranges from 0.0%～0.05%,i.e.no suppression or slightly suppression.The vitrinite reflectance suppression is affected complexly by many factors.The levels of vitrinite reflectance suppression of the source rocks from Dongying Sag having positive relationship with hydrogen index shows that vi-trinite reflectance suppression is closely related to relatively more perhydrous of source rocks.This is consistent with better quality source rocks with high level of vitrinite reflectance suppression.

     

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    • References(16)
  • [1]
    陈家良,邵震杰,秦勇.能源地质学[M].徐州:中国矿业大学出版社,2004.92.
    [2]
    程顶胜.烃源岩有机质成熟度评价方法综述[J].新疆石油地质,1998,19(5):428～432.
    [3]
    孙立中,李显宗,蔡龙珆.混合煤样最大热解峰温与镜质体反射率的研究[J].石油实验地质,2007,29(3):298～300.
    [4]
    王永建,王延斌,郑亚斌等.苏北盆地高邮凹陷泰州组烃源岩演化[J].石油实验地质,2007,29(4):411～414.
    [5]
    Price L C,Barker C E.Suppression of vitrinite reflectance in amorphous rich kerogen—A major unrecognized problem[J].Journal of Petroleum Geology,1985,8(1):59～84.
    [6]
    Wilkins R W T,Wilmshurst J R,Russell N J,et al.Fluorescence alteration and the suppression of vitrinite reflectance[J].Organic Geochemistry,1992,18:629～640.
    [7]
    Wilkins R W T,Wilmshurst J R,Hladky G,et al.Should fluorescence alteration replace vitrinite reflectance as a major tool for thermal maturity determination in oil exploration?[J].Organic Geochemistry,1995,22:191～209.
    [8]
    Hao Fang,Chen Jianyu.The cause and mechanism of vitrinite reflectance anomalies[J].Journal of Petroleum Geology,1992,15(4):419～434.
    [9]
    Lo H B.Correction criteria for the suppression of vitrinite reflectance in hydrogen-rich kerogens:preliminary guidelines[J].Organic Geochemistry,1993,20(6):653～657.
    [10]
    郭迪孝.镜质体反射率是成熟度的通用"标尺"吗?[J].石油实验地质,1990,12(4):421～425.
    [11]
    谢明举,邱楠生.东营凹陷镜质体反射率异常的无机作用探讨[J].西安石油大学学报(自然科学版),2005,20(5):12～16.
    [12]
    张林晔,刘庆,张春荣.东营凹陷成烃与成藏关系研究[M].北京:地质出版社,2005.129～188.
    [13]
    郭汝泰,王建宝,高喜龙等.应用激光探针技术评价烃源岩成熟度:以东营凹陷生油岩研究为例[J].自然科学进展,2003,13(6):626～630.
    [14]
    李志明,秦建中,廖宗廷等.FAMM技术及其应用进展[J].石油实验地质,2005,27(3):307～311.
    [15]
    Davis A,Rathbone R F,Lin R,et al.Observations concerning the nature of maceral fluorescence alteration with time[J].Organic Geochemistry,1990,16:897～906.
    [16]
    Pradier B,Largeau C,Derenne S,et al.Chemical basis of fluorescence alteration of crude oils and kerogens—I.Microfluorimetry of an oil and its isolated fractions:relationships with chemical structure[J].Organic Geochemistry,1990,16:451～460
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