Industrial automation systems and integration - parts library - part 42 : description methodology : methodology for structuring part families 工业自动化系统和集成.零件库.第42部分:描述方法:组构部件系列的方法
Industrial system , installations and equipment and industrial products - structuring principles and reference designations - part 1 : basic rules 工业系统装置和设备及工业产品.组构原理和参考命名.第1部分:基本规则
Structuring principles for technical products and technical product documentation - part 2 : letter codes - main classes and subclasses of objects according to their purpose or task 技术产品和技术产品文献的组构原则.第2部分:字母编码
Industrial systems , installations and equipment and industrial products - structuring principles and reference designations - part 2 : classification of objects and codes for classes 工业系统装置设备和工业产品.组构原理和参考命名.第2部分:对象分类和类别编码
The tectonic stress field indicated by the magnetic fabrics suggested a nw - se compression and shortening , which was consistent with the prediction of the 3d geometric model 磁组构所指示的构造应力场大致为nw - se向挤压缩短，与断层相关褶皱的几何学与运动学模型的预测相一致。
The structure ( fabric and bond ) and structural strength of natural sedimental clays , and the difference and describing methods between natural clays and reconstituted clays are investigated 摘要调查了天然沉积粘土的结构性（组构和胶结） 、结构强度、表述方法以及与重塑土的差异。
These biostromes and bioherms , together with tidal - flat dolomicrite and muddy dolostone , form circum - tidal flat meter - scale carbonate cyclic sequences with symmetrical facies sequences and fabrics 它们与潮坪相泥晶白云岩和泥质白云岩构成具对称相序组构的环潮坪型碳酸盐米级旋回层序。
A right lateral strike slip , which is shown by mapview distribution of the whole fault zone , displacement of the strata , drag folding , s - c fabric and association of subsidiary faults , forms the mainly deformational mechanism 右行走滑活动的主要标志包括断裂带的平面展布、地层错动、牵引褶皱、 s - c组构、次级破裂组合等。
In view of the percentage of void in natural deposit , it is deemed that the increased self - similar rank m can enhance the stability accordingly . and the pattern of stabilization will be non - linear characteristic 随着自相似阶数(对应着颗粒组构的非均匀程度)的增大，堆积体稳定性增强，并得到具有非线性变化特征的稳定性图式。
The immediate host siliceous rocks of typical deposits ( jinya , gaolong ) are of hydrothermal sedimentary origin . gold ore bodies are layer - like and generally concordant with their host rocks . abundant relict synsedimentary fabrics are preserved in the ores 典型矿床(金牙、高龙)中的含矿硅质岩属热水沉积岩，矿体形态主要为与地层整合的层状和似层状，矿石具有大量同生沉积的标型组构。
