1) Jianshi fault
建始断裂
1.
A detailed study of the fractal geometry deformation structure,as well as the latest and present tectonic activity of Jianshi fault has been made to bring to light the kinematic and dynamic characteristics of the fault and its evolution.
本文通过对鄂西建始断裂的几何分形结构和变形结构的分析，结合其新构造活动、现今构造活动特征，探讨断裂的运动学和动力学特征以及形成演化过程。
2) Jianshi-Yushan-Pengshui fault
建始-郁山-彭水断裂
1.
In the Middle-Late Permian,with the open of paleo-tethys,on the regional tension background,the western Hubei provinct(Exi area) was transformed from the gulf into the trough,and developed into an inter-platform rift(trough) in the northestern margin of carbonate platform in the Middle-Upper Yangtze block,which was controlled by Jianshi-Yushan-Pengshui fault.
鄂西地区在中晚二叠世,随着古特提斯洋的打开,在区域性拉伸构造背景控制下,由海湾向海槽转化,并发展成中上扬子碳酸盐台地东北边缘上的一个台间裂陷(槽),它受控于建始-郁山-彭水断裂。
3) incipient break
初始断裂
4) cycle of initiating crack
开始断裂循环数
5) fracture initiation resistance
断裂初始抗力
6) Zhongjiannan Faults
中建南断裂带
补充资料：建始殿
1.古代洛阳宫殿名。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条