himalayan movement meaning in Chinese
喜马拉雅运动
喜马拉雅运支
Examples
- A large scale migration and accumulation took place during later himalayan movement , as a result a type of called remained gas pools with higher gas columns were formed
喜山构造运动使研究区天然气重新大规模运移聚集，形成充满度很高的残余气藏。 - Occurred in the neozoic , the strong himalayan movement made the first order and the second order structure units uplift to form maintains in the basin , which are unfav orable to preserve oil and gas
新生代发生的强烈的喜山运动，促使盆地内部各一、二级正向构造单元进一步冲断上隆、甚至生长为盆内山脉，对古油气藏保存不利。 - The fracture system was mainly made up of vertical fractures which were developed in different phases and showing themselves by plane x - conjugate joint systems . the current fracture character is the result of the himalayan movement
裂缝系统以发育垂直裂缝为主，可形成于不同时期，常成对出现共同组成平n中文摘要面x型共扼剪节理，现今的裂缝性质是喜山期最终作用的结果。 - 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 fault controlled the magmatism and metallization relevant to the contact zone , and deformed successively and produced cataclastic rocks and two sets of joints ; the second stage was from late cretaceous to eocene . the fault zone deformed right - laterally under ne - sw striking transtention , and new joints zone was produced at the end of the two main faults because of local stress concentration . the fault produced inchoative cataclastic rocks , and two sets of typical joints in plutons ; the third stage of deformation was relatively faint and only a little of microcracks was produced and infilled with vei ns in the deformed rocks , which was during the himalayan movement
其后的继承性活动在断裂带内形成碎裂程度最强达到碎裂岩的碎裂岩系列构造岩，变形带两侧发育两组典型的共轭剪节理；第二次在晚白垩世?始新世，断裂在北东?南西向近水平挤压作用下右行张扭性活动，断裂带两主断裂在斜列重叠的端部由于局部应力集中进一步扩展形成节理带，而断裂在岩体区也发育两组典型的共轭剪节理，断裂内形成初碎裂岩为主的构造岩；第三次是喜山期以西侧抬升、东侧下降的强烈升降为主的活动，在基岩中，主断层两侧围岩出现微破裂。