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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2001  >  23(1): 97-102
Zhou Zuyi, R Donelick. MULTIKINETIC MODELLING FOR TIME-TEMPERATURE HISTORY BASED ON APATITE FISSION TRACK DATA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(1): 97-102. doi: 10.11781/sysydz200101097
Citation: Zhou Zuyi, R Donelick. MULTIKINETIC MODELLING FOR TIME-TEMPERATURE HISTORY BASED ON APATITE FISSION TRACK DATA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2001, 23(1): 97-102. doi: 10.11781/sysydz200101097
shu

MULTIKINETIC MODELLING FOR TIME-TEMPERATURE HISTORY BASED ON APATITE FISSION TRACK DATA

doi: 10.11781/sysydz200101097
  • 1.

    MOE Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

  • 2. Department of Geology and Geological Engineering, University of Idaho, Moscow, Idaho 83844, USA

  • Received Date: 2000-09-05
  • Rev Recd Date: 2000-12-12
  • Publish Date: 2001-01-25
    Abstract
  • A new parameter,Dpar,which is the arithmetic mean etch figure diameter parallel to the C-axis at the etched surface,can describe effectively the annealing behavior of apatite fission tracks.Apatite grains from a single sample can be divided into different kinetic populations according to their measured Dpar values.The time-temprature history modelling based on apatite fission track data can therefore be developed into a multikinetic modelling system consisting of several independent apatite thermochronmeters.Consequently,the modelling result is more practical and accurate.Four examples from different Chinese sedimentary basins are shown at the end of the paper.

     

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    • References(14)
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