- 更多网络例句与造陆运动的相关的网络例句 [注：此内容来源于网络，仅供参考]
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After three motions of orogeny and epeirogeny: it lay like a grand dragon of more than 100-km long from east to west in the central plains. It mainly consists of 2parts:h4t.Taishi and Mt. Shaoshi, with each having 36peaks and each peak having name and story, forming colorful natural sceneries.
经过三次造山、造陆运动，需山如一条巨龙横亘在中原大地上，东西绵延百余千米，其主体部分由太室、少室两山组成，各有 36 峰，峰峰有名，峰峰有典，峰峰秀丽，形成了它多彩多姿的自然风光。
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After three motions of orogeny and epeirogeny: it lay like a grand dragon of more than 100- km long f rom east to west in the central plains. It mainly consists of 2parts:h4t.Taishi and Mt. Shaoshi, with each having 36peaks and each peak having name and story, forming colorful natural sceneries.
经过三次造山、造陆运动，需山如一条巨龙横亘在中原大地上，东西绵延百余千米，其主体部分由太室、少室两山组成，各有 36 峰，峰峰有名，峰峰有典，峰峰秀丽，形成了它多彩多姿的自然风光。
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Songshan World Geological Park has a total area of 464square kilometers. In the park, aggradation and structure, such as magmatic rock, metamorphic rock and sedimentary rock of the 5periods of geologic history, namely 二 Archean Eon, Proterozoic Eon, Paleozoic, Mesozoic and Cenozoic, continuously and completely crop out, relics of angular discordance interface and structural feature fwature by 3 global Precambrian orogeny and epeirogeny respectively called SongYang motion, Zhongyue motion and Shaolin motion taking place 25billion years,1.8billion years and 546million years ago. This park is called by geologists as" natural geology museum ,of" five generations under one roof .
嵩山世界地质公园总面积 464 平方千米，公园内连续完整地出露着太古宙、元古宙、古生代、中生代、新生代五个地质历史时期的岩浆岩、变质岩、沉积岩等沉积和构造，清晰地保存着发生在距今 25 亿年、 18 亿年、 5.46 亿年前被分别命名为嵩阳运动、中岳运动和少林运动的三次全球性前寒武纪造山、造陆运动所形成的角度不整合界面及构造形态遗迹，被地质学家称为"五世同堂"的"天然地质博物馆"。
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In the park, aggradation and st ru cture, such as magmatic rock, metamorphic rock and sedimentary rock of the 5periods of geologic history, namely 二 Archean Eon, Proterozoic Eon, Paleozoic, Mesozoic and Cenozoic, continuously and completely crop out, relics of angular discordance interface and structural feature fwature by 3 global Precambrian orogeny and epeirogeny respectively called SongYang motion, Zhongyue motion and Shaolin motion taking place 25billion years,1.8billion years and 546million years ago. This park is called by geologists as" natural geology museum ,of" five generations under one roof .
元古宙、古生代、中生代、新生代五个地质历史时期的岩浆岩、变质岩、沉积岩等沉积和构造，清晰地保存着发生在距今 25 亿年、 18 亿年、 5.46 亿年前被分别命名为高阳运动、中岳运动和少林运动的三次全球性前寒武纪造山、造陆运动所形成的角度不整合界面及构造形态遗迹，被地质学家称为"五世同堂"的"天然地质博物馆"。
- 更多网络解释与造陆运动的相关的网络解释 [注：此内容来源于网络，仅供参考]
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epeirogenesis：造陆运动 造陆作用
epeirocraton 稳定地块陆地克拉通 | epeirogenesis 造陆运动 造陆作用 | epeirogenetic 造陆运动的
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epeirogeny：造陆运动
因此,这类运动过去常称为造陆运动(epeirogeny). 水平运动(horizontal movement)是指地壳或岩石圈物质平行于地表即沿地球切线方向的运动. 常表现为地壳或岩石圈块体的相互分离拉开、相向靠扰挤压或呈剪切平移错动,它可造成岩层的褶皱与断裂,
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epirogeny：造陆作用,造陆运动
造陆的 epirogenic | 造陆作用,造陆运动 epirogeny | 浅钙沸石 episcolecite
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epeirogenetic：造陆的
造礁的;藻珊礁的 hermatypic | 造陆的 epeirogenetic | 造陆运动 continent building
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epeirogenetic：造陆运动的
epeirogenesis 造陆运动 造陆作用 | epeirogenetic 造陆运动的 | epeirogenicearthmovement 造陆运动
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epeirogenic folds：造陆褶皱
epeirogenic earth movement 造陆运动 | epeirogenic folds 造陆褶皱 | epeirogenic movement 造陆运动的
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epeirogenic movement：造陆运动的
epeirogenic earth movement 造陆运动 | epeirogenic movement 造陆运动的 | epeirogenic uplift 造陆上升
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epirogenic movement：造陆运动
epirock 浅带变质岩 | epirogenic movement 造陆运动 | epirogenic 造陆的
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epeirogenic folds：造陆褶皱
epeirogenic earth movement ==> 造陆运动 | epeirogenic folds ==> 造陆褶皱 | epeirogenic movement ==> 造陆运动的
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epeirogenic earth movement：造陆运动
epeiric sea ==> 陆缘海,浅海 | epeirogenic earth movement ==> 造陆运动 | epeirogenic movement ==> 造陆运动的