In this paper, a three-dimensional paleo-geotemperature field equation of sedimentary basin and its initial and boundary conditions are established.

 
  • 為較真實(shí)地反映沉積盆地古地溫的變化情況,建立了適用于不同巖性的沉積盆地地層的古地溫度場(chǎng)方程及其定解條件;
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