【24h】

THE LAST WORD

机译:最后一个字

获取原文
获取原文并翻译 | 示例
           

摘要

Earth is an oblate spheroid, which means its surface curves most at the equator. This means ancient continents that moved from lower to higher latitudes would no longer be shaped to "fit" the curvature of the Earth. Is this effect at all significant and would it be enough to contribute to their breaking up? Is it operational today? 1. Tectonic plates, which cover Earth's surface and carry the continents, are flexible on large scales of time and space (hundreds of thousands of years and thousands of kilometres). This can be seen in the phenomenon of subduction, where one plate is pushed under another, for example the Pacific plate underneath Japan. Friction and mechanical stress during this process lead to volcanism and earthquakes. Another demonstration of tectonic plates' flexibility is the folding of rock to form mountain ranges like the Alps or the Himalayas, which occurs where two tectonic plates collide.
机译:地球是一个扁球体,这意味着它的表面在赤道处弯曲最多。这意味着从低纬度移动到高纬度的古代大陆将不再具有“适应”地球曲率的形状。这种影响是否很明显,足以促进他们的分手?今天可以运作吗? 1.覆盖整个地球表面并承载各大洲的构造板块在较大的时间和空间范围(数十万年数千公里)中具有灵活性。从俯冲现象可以看出这一点,其中一个板块被推到另一个板块之下,例如日本下方的太平洋板块。在此过程中的摩擦和机械应力会导致火山和地震。构造板块灵活性的另一个例证是岩石折叠形成山脉,如阿尔卑斯山或喜马拉雅山,这发生在两个构造板块碰撞的地方。

著录项

  • 来源
    《New scientist》 |2016年第3095期|A1-A1|共1页
  • 作者

  • 作者单位
  • 收录信息 美国《科学引文索引》(SCI);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号