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. 以这些试验现象为依据,提出一个与现有理论不同的关于成岩地质体初始应变能状态的假说。
An explicit boundary type integral formulations of domain variables were presented for three dimensional initial strain problems using boundary element method. 给出了用边界单元法求解三维初应变问题时区域型变量的边界型积分公式的显式。