Volume 5 Issue 3
Jul.  1983
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Zhu Shenzhao, Li Yongxing, Chang Yongying. COLOUR ALTERATION OF FOSSIL SPORO-POLLEN AND THE EVOLUTION OF ORGANIC MATTER[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1983, 5(3): 189-199. doi: 10.11781/sysydz198303189
Citation: Zhu Shenzhao, Li Yongxing, Chang Yongying. COLOUR ALTERATION OF FOSSIL SPORO-POLLEN AND THE EVOLUTION OF ORGANIC MATTER[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1983, 5(3): 189-199. doi: 10.11781/sysydz198303189

COLOUR ALTERATION OF FOSSIL SPORO-POLLEN AND THE EVOLUTION OF ORGANIC MATTER

doi: 10.11781/sysydz198303189
  • Received Date: 1983-07-03
  • Publish Date: 1983-07-25
  • The colour of fossil sporo-pollen is increasingly altered from light to dark with burial depth, pressure and temperature, when the temperature reaches a critical point, original organic matter is transfered into petro leum. Therefore, by means of the colourity of fossil sporo-pollen, the organic alteration stage can be inferred. In Dongpu Depression, on the basis of our research, a conclusion has been reached as follows, For yellow section, underground temperature is 65-93℃, the colour alteration indicates an immature stage. For brown section, 93-125℃, the colour alteration indicates a mature stage. For dark brown section, 125-151℃, the colour alteration indicates a highly-mature stage. For brown-black section, the underground temperature exceeds 151℃, the colour alteration indicates a supermature stage. The study of the colour alteration of fossil sporo-pollen is an important tool for inferring. The evolution of organic matter provides basic information for oil and gas exploration. For this reason, the colour alteration of fossil sporo-pollen can be taken as an indicator of petroleum generation.

     

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