This story, though, raises the question of why there is but a single ejecta layer of iridium and shocked quartz in late Cretaceous rocks around the world.

 
  • 然而,這卻引發(fā)了一個(gè)問(wèn)題:為什么全世界只有一個(gè)白堊紀后期的銥和受震石英熔巖層。
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