《科学》 第391卷 第6791期 · 2026年3月19日 · 中文解读
古老岩石揭示早期板块运动
Ancient rocks reveal early plate motions
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这篇讲什么
本文评论了Brenner等人利用澳大利亚岩石中的古地磁记录,揭示35亿年前地球板块存在差异运动,并表明当时地球磁场稳定且强度与现今相当。
原文开头
Earth had variable tectonic plate motions and a strong, stable magnetic field 3.5 billion years ago Claire Nichols T he movement of tectonic plates—massive slabs of rock—over Earth’s surface controls the planet’s habitability by sustaining the carbon cycle that regulates the climate and stabilizes liquid wa- ter at the surface (1). It also facilitates efficient planetary heat loss, thereby maintaining convection in Earth’s core and the generation of a magnetic field. The presence of a magnetosphere—a space around Earth domi- nated by its magnetic field—provides shielding from solar and cosmic radiation and mediates the loss of atmospheric gas into space (1). …
摘自《科学》(Science)第391卷 第6791期 · 2026年3月19日。仅引用开头一小段供了解文章,版权归原刊所有,全文请阅读原刊。

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