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)。
An explicit boundary type integral formulations of domain variables were presented for three dimensional initial strain problems using boundary element method. 給出了用邊界單元法求解三維初應變問(wèn)題時(shí)區域型變量的邊界型積分公式的顯式。
