燕山运动 meaning in Chinese
yanshan movement
yenshan orogeny
Examples
- The yanshanian orogeny and late mesozoic activation in china continent
燕山运动和中国大陆晚中生代的活化 - The thermal events of late hercynian movement and late yanshanian movement has great effects on the maturation of source rocks
晚海西运动、晚燕山运动对盆地烃源岩的成熟具有重要的影响。 - In himalaya period , the basin was compressed . as tertiary deposits increased , jurassic source rocks started secondary hydrocarbon generation , thus resulting in the activation and reconstruction of the petroleum system
燕山运动中晚期，侏罗系大规模冲隆及剥蚀，侏罗系源岩生烃作用终止，含油气系统被破坏。 - 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。 - During the long course of development , the crustal movement of the " yanshan mountains " raised the seabed above the water and turned it into mountains and valleys . with an uncanny workmanship . nature has carved and shaped this primitive scene of sandstone , forests and valleys , with murmuring streams , fantastic peaks , and grotesque crags
大自然威力无边的“燕山运动” ，将这里逐渐抬升为陆地山脉江河，随后又以挥洒自如的鬼斧神工在这里“穿透切割” “精雕细琢” ，从而有了今天这般个有原始生态体系的砂岩峰林峡谷地貌，构成了溪水潺潺奇峰耸立怪石峥嵘的独特自然景观。