It is shown that regional initial rock stress state is controlled by larger faults and that heterogeneity and aeolotropism of initial rock stress field are caused by superposition of action of faults.
英
美
- 研究結果表明：區域原巖應力狀態(tài)宏觀(guān)上主要受幾何尺寸大的斷層的支配，局部范圍內受復合斷層的疊加擾動(dòng)影響，造成了原巖應力狀態(tài)的各向異性及非均勻分布特征。
