构造叠加 meaning in English
superposition of structures
superpositionofstructures
tectonic superimposing
Examples
- The structural superimposed halo model of quartz - type gold deposits in the xiaoqinling area
小秦岭石英脉型金矿床的构造叠加晕模式 - Forecasting efficiency of structural superimposed halo in the deep of dongtongyu gold mine , shaanxi
构造叠加晕在陕西东桐峪金矿区深部的预测效果 - According to the analysis of the structure deformation variant direction the structure superposition during late period , and the tectonic stress field and deformation variant field , the cover extended nearly sn direction in early stage ( d - c ) , maybe changed the direction in pernian ( especial the late permian ) , and developed some new half - graben along sn direction except the succession activity at great fault zone . the direction of compression deformation variant , however , was nearly sn direction in indo - chinese epoch , ne - sw direction in early yanshan movement epoch , nne - ssw direction in late yanshan movement epoch , and transformed from ew to sn direction in himalayan movement epoch
根据不同构造层中变形方向及后期构造叠加的分析，对本区的构造应力场及变形场进行了探讨，本区盖层早期阶段( d - c )为近南北向的伸展拉张，二叠纪(特别是晚二叠世)的伸展方向可能发生了改变，除在各断裂带继承性活动外，沿南北方向又新生了一些半地堑。而在挤压变形时，印支期主要为近南北向挤压，燕山早期为nw - se向挤压，燕山晚期为nne - ssw向挤压，而喜山运动可能经历了从ew向向sn向方向挤压的转变。 - The dislocation interfaces of early stage were controlled by the slide of the ne fold . the dominant dislocation interfaces , in the dam area , is the one of the second stage , which resulted from the slide of the lava layer and lagerkluftes from nw to se because of the affect of the majiaheba faultage ' s thrusting overriding to the dam area from nw to se . the dislocation interfaces of the third stage were the result of the overprint of the structure of ne to the one of nw
早期阶段形成的错动带受控于北东向纵弯褶皱的层间弯滑机制；第二阶段形成的错动带在坝区占主导地位，它们是由于北东向马家河坝断层由北西向南东的滑脱逆冲推覆影响坝区，并造成坝区向南东缓倾的岩层沿原生构造面向南东滑动的结果；第三阶段形成的错动带则是由于北西向构造叠加于早期北东向构造之上而致。 - The direction of migration was in east and northeast . ( 3 ) this paper introduced the balanced section into the early reservoir description in the sidaogou structure for the first time , and gave a new viewpoint that the sidaogou structure was a fault - bend fold formed by two step thrust fault . the structural stress direction came from the northeast of the hami depression
首次将平衡剖面技术引入了四道沟构造早期油藏描述的构造研究之中，并首次提出四道沟构造是?至少由两个阶梯状断层组成的后倾双重构造叠加的断层转折褶皱，构造应力方向应大致源于北东方向。