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关于克拉通岩石圈破坏的研究进展
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摘要
<正>克拉通是在前寒武纪形成的相对稳定的陆块。克拉通的形成经历了熔体提取作用,富铁的富集组分被移走,相对难熔和缺水的富镁残留体被保存下来(郑永飞和吴福元,2009)。由于镁的密度小于铁,当部分熔融的程度越高,对富铁组分的提取越彻底,残留体的密度就越小,因此,古老的克拉通岩石圈往往密度较低,成为在地球表层长期漂浮的构造块体(吴福元等,2008)。传统观点认为克拉通构成了稳定的核部,供大陆地壳在其基础上增生
引文
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