indo-chinese epoch meaning in English
印支期
Examples
- Sedimentary characteristics and provenance analysis of indo - chinese epoch in the southwest edge of ordos basin
鄂尔多斯盆地西南缘印支期沉积特征及物源 - The first is the depression karst development pattern from dissolution of karst hill during indo - chinese epoch which is the key period for forming space of the reservoir
其中印支早燕山期裸露岩溶属溶丘（梁）洼地型岩溶发育模式，是储集空间形成的重要时期。 - Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part , and belong to the miliangchuan schiefer
矿区所在部位属南秦岭造山带中带古生代伸展盆地叠加印支期冲褶带的北部，隶属于米粮川逆冲岩片。 - The age values are close to crystallizing age of the quartz . combined with other geochronological data and the geological features , it is concluded that the indo - chinese epoch may be the principle mineralization period for gold deposits in the southwestern tianshan mountains . 3
金属硫化物的~ ( 34 ) s = - 3 . 4 + 2 . 6 ，西南天山地区下古生界地层中广泛存在各类火山岩可能是该矿床的主要硫源，部分可能有深部物质的参与。 - 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。