,orogenic peridotite

Dirk Spengler1, Herman L M van Roermund, Martyn R Drury

  • 1Faculteit Geowetenschappen, Universiteit Utrecht, Budapestlaan 4, 3584CD Utrecht, The Netherlands. spengler@geo.uu.nl

Nature
|April 14, 2006
PubMed
概括

这项研究揭示,来自地球深处的古老地幔岩石,通过一次融化事件形成了克拉顿的保护根. 这一发现澄清了这些岩根的起源,以及它们在保存古代大陆地中的作用.

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