我的身体构造英语作文
关于”我身体构造“英语作文模板2篇，作文题目：。以下是关于我身体构造考研英语模板，每篇作文均为满分模板带翻译。
高分英语作文1：
The theory of plate tectoni descbes the movement of the lithosphere. The lithosphere is a relatively hard outer layer of the earth, including all the crust and part of the underlying mantle lithosphere (NIS is divided into dozens of plates of different sizes and shapes. Generally speaking, the plates move each other.
The mid ocean dge is a boundary beeen plates, and new lithosphec mateals are injected fm below As the blocks diverge fm the mid ocean dge, they slide on the yielding layers at the bottom of the lithosphere. Becse the size of the earth is essentially constant, only when the same amount of lithosphec mateal is elsewhere, the site of such destruction is another kind of plate boundary: one plate subducted below the edge of the other plate and re integrated into the mantle. Both plate boundaes are related to flt s, earthquakes and volcanic activity, but the geolo observed at these o boundaes The types of activities are completely different.
The concept of seafloor spreading actually preceded the oginal version of the plate tectoni theory. In the early s, it descbed the formation and destruction of the ocean floor, but it did not specify gid lithosphec plates. This hypothesis was confirmed.
Soon after, as maa se under the mid ocean dge, the peodic rrsal of the earth's maetic field was recorded in the oceanic crust, and the fermaetic minerals in the maa were recorded When the maa cools and solidifies, the fermaetic minerals in the maa will be maetized along the direction of the maa. The direction and polaty of the maetic field are preserved in the maetized volcanic cks. The rrsal of the maetic field pduces a sees of maetic stps parallel to the axis of the ft valley.
Therefore, the oceanic crust can be used as a maetic tape to record the history of geomaetic field, and its width can be determined independently, and the stpe represents the speed of seafloor spreading.
中文翻译：
板块构造理论描述了岩石圈运动，岩石圈是地球一个相对坚硬外层，包括所有地壳和部分下伏地幔岩石圈（nis被分成几十个大小和形状各异板块，一般来说，板块之间是相互运动，大洋中脊是一个板块之间边界，新岩石圈物质从下面注入，当板块从大洋中脊发散时，它们在岩石圈底部较易屈服层上滑动。由于地球大小基上是恒定，只有当相同数量岩石圈物质在其他地方，这种地点是另一种板块边界：一个板块俯冲到另一个板块边缘之下并重新整合到地幔中这两种板块边界都与断层、和火山活动有关，但是，在这两个边界上观察到地质活动种类是完全不同。海底扩张概念实际上先于板块构造理论最初版，在年代早期，它描述了洋底形成和，但它没有具体说明刚岩石圈板块，这一假设得到了证实不久之后，随着岩浆在大洋中脊下上升，在大洋地壳中记录到地球磁场周期反转，岩浆中铁磁矿物被磁化，当岩浆冷却和凝固时，岩浆中铁磁矿物就会沿着岩浆方向磁化，磁场方向和极保存在被磁化火山岩中。
磁场反转产生了一系列平行于裂谷轴线磁条。因此，海洋地壳可以作为一种记录地磁场历史磁带，可以地确定其宽度条纹表示海底扩张速度。
万能作文模板2：
China is the most populous country in the world. Its diverse geological structe and unique multi-ethnic characi attract tousts fm all over the world. For example, the Great Wall, one of the sn wonders of the world, attracts thousands of tousts ry year.
Moreover, China has become one of the fas dloping countes in the world. Businesen are willing to have cheap labor and ch natal resoces to build factoes in China. After 3000 years of struggle, China has opened up to the world and become one of the grea countes in the world.
中文翻译：
是世界上人口最多国家，其多样地质构造和独特多吸引了来自世界各地游客。例如，世界七大奇观之一长城，每年都吸引了成千上万游客，而且已经成为世界上最快发展家之一，商人们愿意有廉价劳动力和丰富自然资源在建厂，经过三奋斗，向世界开放，成为世界上最伟大国家之一。
满分英语范文3：我身体构造
The Himalayas is the highest mountain range in the world. It is located on the southern edge of the Qinghai Tibet Plate, and is the main part of Tibet, China and Pakistan, India, Nepal and Bhutan. It is the junction of China and Nepal.
The west northwest of the Qinghai Tibet Plate is Nanga Parbat. The east of Yarlung Zangbo River is the sharp tning point of nanjabawa. According to the la svey data, Mount Qomolana is Himalayan The average annual increase of cm in the Laya mountains is csed by the collision beeen the Indo Australian plate and the Easian plate.
The Indian plate is still moving northward at a speed of than cm per year. The Himalayas are still sing, and they are also in the collision type seiotectonic zone of plate boundary.
中文翻译：
喜马拉雅山脉是世界上最高山脉，位于青藏高原南缘，位于、和巴基斯坦、印度、尼泊尔和不丹主要部分，是和尼泊尔交界处青藏高原西北偏西南迦帕尔巴特，雅鲁藏布江东至南迦巴瓦急转弯处，长公里，根据最新测量数据，珠穆朗玛峰喜马拉雅山平均每年增加厘米是由印度-澳大利亚板块与欧亚板块碰撞形成印度板块仍以每年超过厘米速度向北移动，喜马拉雅山脉仍在上升，同时也处于板块边界碰撞型构造带。
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