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Chen Zengzhi, Liu Guangdi, Hao Shisheng. A Corrected Method of Using Vitrinite Reflectance Data to Estimate the Thickness of Sediment Removed at an Unconformity[J]. Acta Sedimentologica Sinica, 1999, 17(1): 141-144.
Citation: Chen Zengzhi, Liu Guangdi, Hao Shisheng. A Corrected Method of Using Vitrinite Reflectance Data to Estimate the Thickness of Sediment Removed at an Unconformity[J]. Acta Sedimentologica Sinica, 1999, 17(1): 141-144.

A Corrected Method of Using Vitrinite Reflectance Data to Estimate the Thickness of Sediment Removed at an Unconformity

  • Received Date: 1997-10-14
  • Rev Recd Date: 1998-02-13
  • Publish Date: 1999-03-10
  • Dow(1977) observed that vitrinite reflectance profiles that pass through an unconformity commonly exhibit an offset at the unconformity.And the offset could be used to estimate the amount of missing section.The estimation is accomplished graphically by projecting the preunconformity portion of the profile upward to the point where it attains a value equal to the vitrinite reflectance immediately above the unconformity.The vertical distance between this point and the unconformity was presented as the amount of missing section.This method has been widely used since the late 70's.And its inaccuracy is getting more and more apparent through further application.This paper presents a detailed study on the organic maturation of vitrinite during the burying-uplifting-reburing process.An organic maturity modeling,which integrates complete thermal and burial histories,is used.By the principle of reaction kinetics,it is assuned that the maturation process of the section below the unconformity continues during the erosional phase and the reburial phase.During the reburial phase,the sections above and below the unconformity undergo continued maturation (increases in cumulative TTI values) at different reaction rates,and results in a difference of organic maturation between the two sections. So the difference can be used to trace their burial histories of these sections.And then we proposes a corrected method to estimate the thickness of sediment removed at an unconformity using vitrinite reflectance data of the formations blow and above the unconformity.which can get a more accurate result than Dow's one.
  • [1] 1.李伟恢复地层剥蚀厚度方法综述[期刊论文]-中国海上油气 1996(03)

    2.真柄钦次;童晓光石油圈闭的地质模型 1991

    3.Dow W G Kerogern studies and geological interpretations 1977(01)

    4.Katz B J;Phelfer R N;Schunk D J Interpreation of Discontinuous Vitrinite Reflectance Profiles 1988(08)

    5.Waples D W Time and temperature in petroleum formation:application of Lopatin's method to petroleum exploration1980(08)

    6.Guidish T M;Kendall C C St C;Lerche I Basin evaluation using burial history calculation:an overview 1985(01)

    7.Tissot B P;Pelet R;Ungerer P Thermal History of Sedimentary Basins,Maturation Indices,and Kinetics of Oil and GasGeneration 1987(12)
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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:  1997-10-14
  • Revised:  1998-02-13
  • Published:  1999-03-10

A Corrected Method of Using Vitrinite Reflectance Data to Estimate the Thickness of Sediment Removed at an Unconformity

Abstract: Dow(1977) observed that vitrinite reflectance profiles that pass through an unconformity commonly exhibit an offset at the unconformity.And the offset could be used to estimate the amount of missing section.The estimation is accomplished graphically by projecting the preunconformity portion of the profile upward to the point where it attains a value equal to the vitrinite reflectance immediately above the unconformity.The vertical distance between this point and the unconformity was presented as the amount of missing section.This method has been widely used since the late 70's.And its inaccuracy is getting more and more apparent through further application.This paper presents a detailed study on the organic maturation of vitrinite during the burying-uplifting-reburing process.An organic maturity modeling,which integrates complete thermal and burial histories,is used.By the principle of reaction kinetics,it is assuned that the maturation process of the section below the unconformity continues during the erosional phase and the reburial phase.During the reburial phase,the sections above and below the unconformity undergo continued maturation (increases in cumulative TTI values) at different reaction rates,and results in a difference of organic maturation between the two sections. So the difference can be used to trace their burial histories of these sections.And then we proposes a corrected method to estimate the thickness of sediment removed at an unconformity using vitrinite reflectance data of the formations blow and above the unconformity.which can get a more accurate result than Dow's one.

Chen Zengzhi, Liu Guangdi, Hao Shisheng. A Corrected Method of Using Vitrinite Reflectance Data to Estimate the Thickness of Sediment Removed at an Unconformity[J]. Acta Sedimentologica Sinica, 1999, 17(1): 141-144.
Citation: Chen Zengzhi, Liu Guangdi, Hao Shisheng. A Corrected Method of Using Vitrinite Reflectance Data to Estimate the Thickness of Sediment Removed at an Unconformity[J]. Acta Sedimentologica Sinica, 1999, 17(1): 141-144.
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