1) hercynian orogeny
海戊山运动
2) Hercynian orogeny
海西期造山运动
3) Subhercynian orogeny
新海西造山运动
4) Yanshan movement
燕山运动
1.
Jurassic Tectonic Revolution in China and New Interpretation of the Yanshan Movement;
中国侏罗纪构造变革与燕山运动新诠释
2.
The Indo-Chinese movement and Yanshan movement were two important tectonic movements in the Mesozoic era.
中生代印支运动和燕山运动是对济阳坳陷有重大改造的2次构造运动,印支期主要发育NW向逆推断层,燕山早期则为逆断层向正断层的过渡阶段,燕山中、晚期NW向断层发生构造反转,由逆断层转换为正断层。
3.
The effect of Yanshan movement and Himalayan orogeny on hydrocarbon migration and accumulation in Junggar basin is analyzed.
分析了燕山运动和喜马拉雅运动在准噶尔盆地油气运移和聚集中的作用。
5) Himalayan movement
喜山运动
1.
By analyzing tectonic activities,hydrocarbon source-reservoir-seal associations and crude geochemistry in Laizhouwan sag,it is considered that the main tectonic events to control hydrocarbon accumulation are Himalayan movement and Tanlu Fault activity.
通过对莱州湾凹陷构造活动、生储盖组合及所发现原油地球化学特征的分析,认为影响该区油气成藏的构造活动主要为喜山运动和郯庐断裂活动。
6) orogenic movement
造山运动
1.
Indosinian movement was a strong pressed folding orogenic movement in company with magma activity, which was dominated by N-S direction compression.
印支期地壳以南北向挤压作用为主 ,是一次强烈褶皱造山运动 ,并伴随有强烈的岩浆活动。
补充资料：南美洲运动会和南十字运动会
1922年在巴西举行过1届南美洲运动会,参加者限于南美洲国家。1978年在玻利维亚举行过 1届南十字运动会，参加国有阿根廷、玻利维亚、巴西、智利、厄瓜多尔、巴拉圭、秘鲁和乌拉圭8国。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条