yanshan movement meaning in Chinese
燕山运动
Examples
- Through research , the organic matter of source rocks in carboniferous - permian coal measure strata began first hydrocarbon - generating in mesozoic , and the first hydrocarbon - filling took place . but , because of yanshan movement later , the carboniferous - permian strata rose , as a result , the first hydrocarbon - generating and reservoir - forming paused ; in early tertiary period , because carboniferous - permian strata dipping forward east originally turned into dipping forward west , the prototype of faulted block began to form gradually ; by the end of sha - 3 period of early tertiary , the paleogeotherm of carboniferous - permian strata exceed the mesozoic ' s temperature again , and accordingly , abundant hydrocarbon was generated and expulsed secondly . the trap continued to develop ; from the end of late tertiary to quaternary , the second hydrocarbon - generating and expulsing got to its peak , and the second reservoir - forming was over
研究表明，本区石炭?二叠纪烃源岩在中生代发生一次生烃和排烃，并有油气充注，后因燕山运动导致地层抬升，一次生烃和成藏过程中止；在早第三纪，原来东倾的地层变为西倾，断块圈闭开始具雏形；至早第三纪沙二末期，石炭?二叠系的大部分地层古地温再次超过中生代一次生烃的温度，开始二次生烃和排烃，圈闭持续发育；晚第三纪末?第四纪，二次生烃、排烃达到高峰，二次成藏完成。 - 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。 - Based on the analysis of the data on global metallogeny in the framework of geodynamics and study of the processes of continental evolution and metalloeny of of sanjiang , qinling and xingan - mongolia orogenic belts , we have reconsidered the geodynamic evlution and metallogeny during indosinian to early - yanshan movement in china , and established large - scale metallogenic model on intracontinental evolution we in orogenic belts . the main results are summarized as follow . ( 1 ) systematically gathering the data about large - scale and superlarge - scale deposits in the world and drawing up the map of global tectonics and metallogeny ; finding out the segmentation of circle - pacific ocean metallogenic belt and informing that the giant deposit clusters are the prominent feature of global metallogeny
本文在总结全球大规模成矿的地球动力学背景资料基础上，通过深入解剖和系统对比我国三江造山带南段、东秦岭造山带和兴蒙造山带中南部等典型造山带关键地区以陆内演化过程为核心的地球动力学演化历史及其成矿特征，重新认识了我国大陆印支?早燕山期的动力学演化过程及其成矿效应，建立了关于造山带陆内演化阶段主要过程中的大规模成矿模式。 - There existed several strong reformation of late - yanshan movement and himalaya movement the generation , development , disappearance and reformation are tightly related to tarim block , tianshan belt and tethyan tectonic zone , especially tianshan belt , which makes the great difference between present and original basin
该盆地形成后经历了燕山晚期和喜山期构造运动的多期强烈改造；其产生、发展和消亡以及改造与塔里木地块、天山构造带、特提斯构造域的演化息息相关。其中尤以天山构造带的活动影响最大，从而造就盆地今古面貌差异巨大。 - The yanshan - liaoning area is called as the " cradle of geology " . it is the first time that the geologist , wen wenghao , has put forward the " yanshan movement " before 70 years . from then on the yanshan - liaoning area had been paying attention by the geologists all over the word because it lies in the particular tectonic background , has the complex structural features , structural units , and the geological history of evolution , particularly large - scale , multi - phrase tectonic movement and magmatic activity took place in the short geological time
燕辽地区素有地质“摇篮”之称，自翁文灏在70余年前提出yenshanmovement (燕山运动)以来，它以其独特的大地构造位置、复杂的构造特征、组成及其演化过程，特别是该地区在很短的时间间隔内发生了大规模、多幕式构造?岩浆活动，更引起世界地学界的极大关注。