Based on the observed phenomena, a hypothesis on the original state of strain energy in a geological body after diagenesis, which is different from present theories, is advanced.

 
  • 以這些試驗現象為依據,提出一個(gè)與現有理論不同的關(guān)于成巖地質(zhì)體初始應變能狀態(tài)的假說(shuō)。
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