The diagenetic stages and diagenetic facies are predicted by modeling the paleotemperature, vitrinite reflectance, sterane isomerization rate and authigenic quartz concentration in space and time.

 
  • 該文通過(guò)模擬古地溫、鏡質(zhì)組反射率、甾烷異構化率和自生石英含量隨時(shí)間的變化規律,預測了西部凹陷南段成巖階段和成巖相的橫向展布。
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