1) rock macroscope deformation
岩石宏观变形
2) macroscopic deformation
宏观形变
3) macro-deformation
宏观变形
1.
Two diffusion bonding techniques: transient liquid phase diffusion bonding and hot isostatic pressing diffusion bonding was brought in and the macro-deformation of the diffusion bonding jionts was solved.
连接温度限制的条件下,压力是影响扩散连接的最主要参数,为保证扩散连接的快速进行,通常需要较大的连接压力,焊件的宏观变形就成为扩散连接的主要问题。
4) rock deformation
岩石变形
1.
The influence of rock deformation on the crystallinity of clay minerals: a case study of the Jinshan gold deposit in Jiangxi Province;
岩石变形对粘土矿物结晶生长影响的初步研究——以江西金山金矿为例
2.
Experiment on sample simulation for detecting rock deformation by fiber optic grating;
光纤光栅测试岩石变形的试件模拟实验研究
3.
Considered rock deformation and natural water influx into over-pressured reservoirs, a modified material balance equation was derived b.
根据气藏各个压降阶段气藏束缚水体积膨胀方程和不稳定水侵方程,推导出考虑岩石变形及自然水侵的异常高压有水气藏物质平衡方程,并通过试算法给出了方程的解。
5) deformed rocks
变形岩石
1.
X-ray fabric analysis of deformed rocks in the eastern part of the Fuyun-Qinghe area, Altay, Xinjiang, China;
阿尔泰富蕴—青河一带东段变形岩石X光组构分析
2.
Based on the Xray petrofabrics analysis of deformed rocks from Beishan area, Gansu, the authors draw the conclusion as follows.
通过对甘肃北山地区变形岩石的X光岩组分析,得知该区岩石变形比较强烈。
6) macroscopic lattice deformation
宏观点阵变形
1.
The macroscopic lattice deformation characteristics of four kinds of typical martensite transformation in iron-based alloy were observed and quantitatively analyzed by means of atomic force microscope (AFM), and it showed that the macroscopic lattice deformation characteristics of these four kinds of typical martensite transformation are not the same.
利用原子力显微镜观察并定量分析了铁基合金4种典型惯习面马氏体相变的宏观点阵变形特征。
补充资料：岩石变形模量
岩石变形模量
deformation modulus of rock
yanshlb一anx一ngl下旧1一ang岩石变形模里(deformation modulus of roek) 指强度极限范围内的岩石应力应变之比。是岩石物理力学性质之一。在作反复加卸载试验时，岩石的总变形包括弹性变形和永久变形两个部分。岩石的变形模量ED为加在岩石上的应力与总变形之比，即 J八 百「一— 一’￡。十Cp式中氏为岩石所受的应力;‘为岩石的可恢复变形;哪为岩石的不可恢复变形。 (周昌达)
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