1) Embryonic fracture
雏形断裂
1.
During the process of studying tectonic origin of Gold-bearing breccia bodies in the Shuangwang gold deposit ,Shanxi province, the author apply several modern tectonics theories, such as hydrofracturing, fluid dynamic breccia, tectonic pumping, deformation partitioning, embryonic fracture etc.
本文所探讨的陕西双王含金角砾岩体的构造成因研究运用了水力压裂作用、流体动力角砾岩、流体泵吸作用、变形分解作用和雏形断裂理论等几个现代构造地质理论，提出了变形分解作用—雏形断裂作用—水力压裂作用—裂开愈合作用四位一体的水压角砾岩型咸矿构造模型，是与流体动力作用有关的裂隙—脉—角砾岩系成矿构造的一种新的模式。
3) cracking deformation
断裂变形
1.
Based on the theoretic solution of cracking deformation,the calculation equations for the maximum dynamic load stress and the residual stress after cracking are given in this paper.
与经典的小变形理论不同,本研究工作使用大变形理论公式描述断裂变形,并用各个增量断裂变形的乘积描述最终的系列断裂作用。
4) arcuate fault
弧形断裂
1.
Based on researches on characteristics of the He125 fault,the authors have found that the arcuate fault is parallel to the fault strike and is the combination of fault-trough and fault-ridge,as evidenced from the profile.
通过对河125断层几何学特征的分析发现弧形断裂平行于断层走向剖面上表现为断槽、断脊组合;垂直于断层走向剖面上断层分为竖滑段、倾滑段和平滑段3段,生长指数规律为弧中大于弧翼,断层倾角规律为弧中小于弧翼。
2.
The arcuate fault is the combination of fault trough and fault ridge,it is found from the section that is parallel to the arcuate,the fault can be separately divided into three parts,vertical-slip part,dip-slip part and horizontal-slip part from the section that is perpendicula.
为解释断层下降盘浊积砂体横向不均一的控制机理,从河125断层几何特征入手,剖析了断层形态与浊积砂体的关系,发现弧形断裂平行于断层走向剖面上为断槽、断脊组合;在垂直于断层走向剖面上断层可分为竖滑段、倾滑段和平滑段三段。
5) subulate fracture
锥形断裂
6) fracture morphology
断裂形态
1.
Tensile yield strength was used to quantitatively evaluate the interfacial interactions,which have significant influence on the tensile fracture morphology of the composites.
采用拉伸屈服强度定量表征了界面相互作用的强弱,研究了界面相互作用对三元复合体系拉伸断裂形态的影响。
2.
The properties of compounds and vulcanizates of SSBR/NR blend,as well as the fracture morphology of vulcanizates of SSBR/NR blend were studied.
研究了不同共混比的锡偶联型溶聚丁苯橡胶/天然橡胶 (SSBR/NR)共混物的生胶及硫化胶的性能及断裂形态。
补充资料：雏形
解释：
名词：未定型前的形式，依照原物缩小的模型。
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