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LI Hui jun, WU Tai ran, HAO Yin quan, ZHANG Xiu zhu, MA Zong jin. Overpressure Retardation of Organic Matter and Its Significance for Petroleum Geology[J]. Acta Sedimentologica Sinica, 2004, 22(4): 737-742.
Citation: LI Hui jun, WU Tai ran, HAO Yin quan, ZHANG Xiu zhu, MA Zong jin. Overpressure Retardation of Organic Matter and Its Significance for Petroleum Geology[J]. Acta Sedimentologica Sinica, 2004, 22(4): 737-742.

Overpressure Retardation of Organic Matter and Its Significance for Petroleum Geology

  • Received Date: 2003-12-01
  • Rev Recd Date: 2004-05-13
  • Publish Date: 2004-12-10
  • Overpressure developed in Banqiao Sag, Eastern China, and obvious overpressure retardation of organic matter maturation was found in Well BS35. Such an organic matter maturity anomaly is distinctly different from those caused by variation in activation energies, conductivity contrasts, and hydrologic effects. Overpressure retardation has been proven to be conditional through integrated organic geochemical and geologic research, early developed overpressure, high original TOC contents of source rocks and the retention of the pore fluids (including products of organic matter maturation reactions) in the source rocks are three important factors affecting overpressure retardation of organic matter maturation, and overpressure retardation of organic matter maturation is quite important for clearly understanding petroleum exploration during deep burial in overpressured sedimentary basins.
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  • Received:  2003-12-01
  • Revised:  2004-05-13
  • Published:  2004-12-10

Overpressure Retardation of Organic Matter and Its Significance for Petroleum Geology

Abstract: Overpressure developed in Banqiao Sag, Eastern China, and obvious overpressure retardation of organic matter maturation was found in Well BS35. Such an organic matter maturity anomaly is distinctly different from those caused by variation in activation energies, conductivity contrasts, and hydrologic effects. Overpressure retardation has been proven to be conditional through integrated organic geochemical and geologic research, early developed overpressure, high original TOC contents of source rocks and the retention of the pore fluids (including products of organic matter maturation reactions) in the source rocks are three important factors affecting overpressure retardation of organic matter maturation, and overpressure retardation of organic matter maturation is quite important for clearly understanding petroleum exploration during deep burial in overpressured sedimentary basins.

LI Hui jun, WU Tai ran, HAO Yin quan, ZHANG Xiu zhu, MA Zong jin. Overpressure Retardation of Organic Matter and Its Significance for Petroleum Geology[J]. Acta Sedimentologica Sinica, 2004, 22(4): 737-742.
Citation: LI Hui jun, WU Tai ran, HAO Yin quan, ZHANG Xiu zhu, MA Zong jin. Overpressure Retardation of Organic Matter and Its Significance for Petroleum Geology[J]. Acta Sedimentologica Sinica, 2004, 22(4): 737-742.
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